G4021 Igneous petrology
Faculty of ScienceAutumn 2024
- Extent and Intensity
- 2/1/0. 5 credit(s). Type of Completion: zk (examination).
In-person direct teaching - Teacher(s)
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat. (lecturer)
Petra Ludvová Hašková, DiS. (assistant) - Guaranteed by
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: Ing. Jana Pechmannová
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science - Timetable
- Tue 12:00–13:50 G1,01004, Tue 14:00–14:50 G1,01004
- Prerequisites
- (PROGRAM(KOS)|| G3021k Petrography || G3021 Petrography ) && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE4)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemical substances )))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 78 student(s).
Current registration and enrolment status: enrolled: 9/78, only registered: 0/78, only registered with preference (fields directly associated with the programme): 0/78 - fields of study / plans the course is directly associated with
- there are 32 fields of study the course is directly associated with, display
- Course objectives
- The course aims to the genesis of the most important rock groups.
- Learning outcomes
- At the end of this course, students should be able to: understand problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Literature
- HALL, Anthony. Igneous petrology. 2nd ed. Essex: Longman Group, 1996, xiv, 551. ISBN 0582230802. info
- WINTER, John D. An introduction to igneous and metamorphic petrology. 2nd ed. Upper Saddle River, N.J.: Prentice Hall, 2010, xviii, 702. ISBN 9780321592576. info
- BEST, Myron G. Igneous petrology. Malden, Massachusetts: Blackwell Science, 2001, xvi, 458 s. ISBN 0-86542-541-8. info
- KONOPÁSEK, Jiří. Metamorfní petrologie. 1. vyd. Praha: Karolinum, 1998, 241 s. ISBN 8071846686. info
- MCLANE, Michael. Sedimentology. New York: Oxford University Press, 1995, xiii, 423. ISBN 0195078683. info
- BLATT, Harvey. Sedimentary petrology. 2nd ed. New York: W.H. Freeman, 1992, 514 s. ISBN 0716722739. info
- Teaching methods
- lecture
- Assessment methods
- Lectures, written tests
- Language of instruction
- Czech
- Further comments (probably available only in Czech)
- Study Materials
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2024/2025.
G4021 Igneous petrology
Faculty of ScienceAutumn 2022
- Extent and Intensity
- 2/1/0. 5 credit(s). Type of Completion: zk (examination).
- Teacher(s)
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat. (lecturer)
Petra Ludvová Hašková, DiS. (assistant) - Guaranteed by
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science - Timetable
- Tue 13:00–14:50 G1,01004, Tue 15:00–15:50 G1,01004
- Prerequisites
- (PROGRAM(KOS)|| G3021k Petrography || G3021 Petrography ) && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE4)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemical substances )))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 78 student(s).
Current registration and enrolment status: enrolled: 2/78, only registered: 0/78, only registered with preference (fields directly associated with the programme): 0/78 - fields of study / plans the course is directly associated with
- there are 32 fields of study the course is directly associated with, display
- Course objectives
- The course aims to the genesis of the most important rock groups.
- Learning outcomes
- At the end of this course, students should be able to: understand problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Literature
- HALL, Anthony. Igneous petrology. 2nd ed. Essex: Longman Group, 1996, xiv, 551. ISBN 0582230802. info
- WINTER, John D. An introduction to igneous and metamorphic petrology. 2nd ed. Upper Saddle River, N.J.: Prentice Hall, 2010, xviii, 702. ISBN 9780321592576. info
- BEST, Myron G. Igneous petrology. Malden, Massachusetts: Blackwell Science, 2001, xvi, 458 s. ISBN 0-86542-541-8. info
- KONOPÁSEK, Jiří. Metamorfní petrologie. 1. vyd. Praha: Karolinum, 1998, 241 s. ISBN 8071846686. info
- MCLANE, Michael. Sedimentology. New York: Oxford University Press, 1995, xiii, 423. ISBN 0195078683. info
- BLATT, Harvey. Sedimentary petrology. 2nd ed. New York: W.H. Freeman, 1992, 514 s. ISBN 0716722739. info
- Teaching methods
- lecture
- Assessment methods
- Lectures, written tests
- Language of instruction
- Czech
- Further comments (probably available only in Czech)
- Study Materials
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2022/2023.
G4021 Igneous petrology
Faculty of ScienceAutumn 2020
- Extent and Intensity
- 2/1. 5 credit(s). Type of Completion: zk (examination).
- Teacher(s)
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat. (lecturer)
Petra Ludvová Hašková, DiS. (assistant) - Guaranteed by
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science - Timetable
- Tue 12:00–13:50 G1,01004, Tue 14:00–14:50 G1,01004; and Thu 20. 5. 8:00–13:00 G1,01004
- Prerequisites
- (PROGRAM(KOS)|| G3021k Petrography || G3021 Petrography ) && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE4)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 78 student(s).
Current registration and enrolment status: enrolled: 0/78, only registered: 0/78, only registered with preference (fields directly associated with the programme): 0/78 - fields of study / plans the course is directly associated with
- there are 32 fields of study the course is directly associated with, display
- Course objectives
- The course aims to the genesis of the most important rock groups.
- Learning outcomes
- At the end of this course, students should be able to: understand problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Literature
- Teaching methods
- lecture
- Assessment methods
- Lectures, written tests In the case of a crisis pandemic situation, the course will be completed in the autumn semester of 2020 by distance form.
- Language of instruction
- Czech
- Further comments (probably available only in Czech)
- Study Materials
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2020/2021.
G4021 Igneous petrology
Faculty of ScienceAutumn 2018
- Extent and Intensity
- 2/1/0. 5 credit(s). Type of Completion: zk (examination).
- Teacher(s)
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat. (lecturer)
- Guaranteed by
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science - Timetable
- Mon 17. 9. to Fri 14. 12. Tue 14:00–15:50 G1,01004, Tue 16:00–16:50 G1,01004
- Prerequisites
- (PROGRAM(KOS)|| G3021k Petrology I || G3021 Petrology I ) && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE4)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 78 student(s).
Current registration and enrolment status: enrolled: 0/78, only registered: 0/78, only registered with preference (fields directly associated with the programme): 0/78 - fields of study / plans the course is directly associated with
- there are 32 fields of study the course is directly associated with, display
- Course objectives
- The course aims to the genesis of the most important rock groups.
- Learning outcomes
- At the end of this course, students should be able to: understand problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Literature
- Teaching methods
- lecture
- Assessment methods
- Lectures, written tests
- Language of instruction
- Czech
- Further comments (probably available only in Czech)
- The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2018/2019.
G4021 Igneous and metamorphic petrology (II)
Faculty of ScienceAutumn 2016
- Extent and Intensity
- 2/0. 3 credit(s). Type of Completion: graded credit.
- Teacher(s)
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat. (lecturer)
Mgr. David Buriánek, Ph.D. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Mgr. Vojtěch Wertich, Ph.D. (seminar tutor) - Guaranteed by
- doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science - Timetable
- Mon 19. 9. to Sun 18. 12. Tue 15:00–16:50 G2,02003
- Prerequisites
- (PROGRAM(KOS)|| G3021k Petrology I || G3021 Petrology I ) && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE4)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 80 student(s).
Current registration and enrolment status: enrolled: 0/80, only registered: 0/80, only registered with preference (fields directly associated with the programme): 0/80 - fields of study / plans the course is directly associated with
- there are 14 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: understand problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Sedimentary rocks:
- Rock-forming minerals of sedimentary rocks - origin and petrogenesis: clay minerals, silicon oxides and hydroxides, feldspars, carbonates, phosphates, oxides, Fe, Mn, Al-hydroxides, sulfates, chlorides, iron sulfides. Organic matters. Rock-forming organism.
- Origin and evolution of sedimentary structures: Textural characteristic (distribution of grain size, the shapes of sedimentary particles, surface texture of sedimentary particles, matrix, cements and cementation, ooids and pisoids, spherulitic texture, primary and secondary porosity, permeability). Textural classification. Structural classification of sedimentary rocks. Outer and inner structures.
- Origin of sedimentary rocks: weathering processes (mechanical and chemical degradation of rocks, sedimentary cycle, soil formation, erosion. Transport (medium motion, grain flows, water transport, eolian transport, glacial and gravitational processes, orientation of grains). Sedimentation, types of deposition environments. Influence of the tectonic and climatic conditions, sedimentation velocity. Maturity of sediments. Diagenesis of sediments, diagenetic evolution (syndiagenesis, anadiagenesis, epidiagenesis), main phases arising during lithogenesis, geophysical and geochemical conditions of diagenesis, Diagenetic metasomatism. Anchimetamorphism.
- Recent sediments.
- Metamorphic rocks
- Individual types of metamorphic rocks will be treated with emphasis on the geotectonic setting of their genesis. Methods of metamorphic rocks studies aiming at determination of P-T conditions of their formation will be presented. This will include analyses of relationships between metamorphism and deformation, formation and use of mineral zoning, geothermobarometry, geochronology, petrogenetic grids and metamorphic P-T paths. Examples from the Bohemian Massif will be presented.
- 1. Metapelites, quartzofeldspathic rocks (orthogneisses)
- 2. Metabasic and mafic rocks.
- 3. Metacarbonates, calc-silicate rocks .
- 4. High temperature and ultra-high temperature metamorphism, low, medium and high pressure granulites, anatexis, contact metamorphism.
- Literature
- HALL, Anthony. Igneous petrology. 2nd ed. Essex: Longman Group, 1996, xiv, 551. ISBN 0582230802. info
- MCLANE, Michael. Sedimentology. New York: Oxford University Press, 1995, xiii, 423. ISBN 0195078683. info
- BLATT, Harvey. Sedimentary petrology. 2nd ed. New York: W.H. Freeman, 1992, 514 s. ISBN 0-7167-2273-9. info
- KUKAL, Zdeněk. Základy sedimentologie. 1. vyd. Praha: Academia, 1986, 466 s. info
- KUKAL, Zdeněk. Geology of recent sediments. Praha: Academia, 1970, 490 s. info
- KONOPÁSEK, Jiří. Metamorfní petrologie. 1. vyd. Praha: Karolinum, 1998, 241 s. ISBN 8071846686. info
- BEST, Myron G. Igneous petrology. Malden, Massachusetts: Blackwell Science, 2001, xvi, 458 s. ISBN 0-86542-541-8. info
- Teaching methods
- lecture
- Assessment methods
- Lectures, written tests
- Language of instruction
- Czech
- Further comments (probably available only in Czech)
- Study Materials
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2016/2017.
G4021 Igneous and metamorphic petrology (II)
Faculty of ScienceAutumn 2014
- Extent and Intensity
- 2/0. 3 credit(s). Type of Completion: graded credit.
- Teacher(s)
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat. (lecturer)
Mgr. David Buriánek, Ph.D. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Mgr. Jakub Haifler, Ph.D. (seminar tutor), doc. RNDr. Jana Kotková, CSc. (deputy)
Mgr. Vojtěch Wertich, Ph.D. (seminar tutor) - Guaranteed by
- doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science - Timetable
- Thu 8:00–9:50 G1,01004
- Prerequisites
- ( G3021k Petrology I || G3021 Petrology I ) && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE4)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 150 student(s).
Current registration and enrolment status: enrolled: 0/150, only registered: 0/150, only registered with preference (fields directly associated with the programme): 0/150 - fields of study / plans the course is directly associated with
- there are 14 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: understand problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Sedimentary rocks:
- Rock-forming minerals of sedimentary rocks - origin and petrogenesis: clay minerals, silicon oxides and hydroxides, feldspars, carbonates, phosphates, oxides, Fe, Mn, Al-hydroxides, sulfates, chlorides, iron sulfides. Organic matters. Rock-forming organism.
- Origin and evolution of sedimentary structures: Textural characteristic (distribution of grain size, the shapes of sedimentary particles, surface texture of sedimentary particles, matrix, cements and cementation, ooids and pisoids, spherulitic texture, primary and secondary porosity, permeability). Textural classification. Structural classification of sedimentary rocks. Outer and inner structures.
- Origin of sedimentary rocks: weathering processes (mechanical and chemical degradation of rocks, sedimentary cycle, soil formation, erosion. Transport (medium motion, grain flows, water transport, eolian transport, glacial and gravitational processes, orientation of grains). Sedimentation, types of deposition environments. Influence of the tectonic and climatic conditions, sedimentation velocity. Maturity of sediments. Diagenesis of sediments, diagenetic evolution (syndiagenesis, anadiagenesis, epidiagenesis), main phases arising during lithogenesis, geophysical and geochemical conditions of diagenesis, Diagenetic metasomatism. Anchimetamorphism.
- Recent sediments.
- Metamorphic rocks
- Individual types of metamorphic rocks will be treated with emphasis on the geotectonic setting of their genesis. Methods of metamorphic rocks studies aiming at determination of P-T conditions of their formation will be presented. This will include analyses of relationships between metamorphism and deformation, formation and use of mineral zoning, geothermobarometry, geochronology, petrogenetic grids and metamorphic P-T paths. Examples from the Bohemian Massif will be presented.
- 1. Metapelites, quartzofeldspathic rocks (orthogneisses)
- 2. Metabasic and mafic rocks.
- 3. Metacarbonates, calc-silicate rocks .
- 4. High temperature and ultra-high temperature metamorphism, low, medium and high pressure granulites, anatexis, contact metamorphism.
- Literature
- HALL, Anthony. Igneous petrology. 2nd ed. Essex: Longman Group, 1996, xiv, 551. ISBN 0582230802. info
- MCLANE, Michael. Sedimentology. New York: Oxford University Press, 1995, xiii, 423. ISBN 0195078683. info
- BLATT, Harvey. Sedimentary petrology. 2nd ed. New York: W.H. Freeman, 1992, 514 s. ISBN 0-7167-2273-9. info
- KUKAL, Zdeněk. Základy sedimentologie. 1. vyd. Praha: Academia, 1986, 466 s. info
- KUKAL, Zdeněk. Geology of recent sediments. Praha: Academia, 1970, 490 s. info
- KONOPÁSEK, Jiří. Metamorfní petrologie. 1. vyd. Praha: Karolinum, 1998, 241 s. ISBN 8071846686. info
- BEST, Myron G. Igneous petrology. Malden, Massachusetts: Blackwell Science, 2001, xvi, 458 s. ISBN 0-86542-541-8. info
- Teaching methods
- lecture
- Assessment methods
- Lectures, written tests
- Language of instruction
- Czech
- Further comments (probably available only in Czech)
- Study Materials
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2014/2015.
G4021 Igneous and metamorphic petrology (II)
Faculty of ScienceAutumn 2012
- Extent and Intensity
- 2/0. 3 credit(s). Type of Completion: graded credit.
- Teacher(s)
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat. (lecturer)
Mgr. David Buriánek, Ph.D. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer) - Guaranteed by
- doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science - Timetable
- Mon 8:00–9:50 Bp1,01007
- Prerequisites
- ( G3021k Petrology I || G3021 Petrology I ) && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE4)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 36 student(s).
Current registration and enrolment status: enrolled: 0/36, only registered: 0/36, only registered with preference (fields directly associated with the programme): 0/36 - fields of study / plans the course is directly associated with
- there are 14 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: understand problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Sedimentary rocks:
- Rock-forming minerals of sedimentary rocks - origin and petrogenesis: clay minerals, silicon oxides and hydroxides, feldspars, carbonates, phosphates, oxides, Fe, Mn, Al-hydroxides, sulfates, chlorides, iron sulfides. Organic matters. Rock-forming organism.
- Origin and evolution of sedimentary structures: Textural characteristic (distribution of grain size, the shapes of sedimentary particles, surface texture of sedimentary particles, matrix, cements and cementation, ooids and pisoids, spherulitic texture, primary and secondary porosity, permeability). Textural classification. Structural classification of sedimentary rocks. Outer and inner structures.
- Origin of sedimentary rocks: weathering processes (mechanical and chemical degradation of rocks, sedimentary cycle, soil formation, erosion. Transport (medium motion, grain flows, water transport, eolian transport, glacial and gravitational processes, orientation of grains). Sedimentation, types of deposition environments. Influence of the tectonic and climatic conditions, sedimentation velocity. Maturity of sediments. Diagenesis of sediments, diagenetic evolution (syndiagenesis, anadiagenesis, epidiagenesis), main phases arising during lithogenesis, geophysical and geochemical conditions of diagenesis, Diagenetic metasomatism. Anchimetamorphism.
- Recent sediments.
- Metamorphic rocks
- Individual types of metamorphic rocks will be treated with emphasis on the geotectonic setting of their genesis. Methods of metamorphic rocks studies aiming at determination of P-T conditions of their formation will be presented. This will include analyses of relationships between metamorphism and deformation, formation and use of mineral zoning, geothermobarometry, geochronology, petrogenetic grids and metamorphic P-T paths. Examples from the Bohemian Massif will be presented.
- 1. Metapelites, quartzofeldspathic rocks (orthogneisses)
- 2. Metabasic and mafic rocks.
- 3. Metacarbonates, calc-silicate rocks .
- 4. High temperature and ultra-high temperature metamorphism, low, medium and high pressure granulites, anatexis, contact metamorphism.
- Literature
- Teaching methods
- lecture
- Assessment methods
- Lectures, written tests
- Language of instruction
- Czech
- Further comments (probably available only in Czech)
- Study Materials
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2012/2013.
G4021 Igneous and metamorphic petrology (II)
Faculty of ScienceAutumn 2010
- Extent and Intensity
- 2/0. 3 credit(s). Type of Completion: graded credit.
- Teacher(s)
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat. (lecturer)
Mgr. David Buriánek, Ph.D. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer) - Guaranteed by
- doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr. - Timetable
- Tue 12:00–13:50 G1,01004
- Prerequisites
- ( G3021k Petrology I || G3021 Petrology I ) && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE4)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 80 student(s).
Current registration and enrolment status: enrolled: 0/80, only registered: 0/80, only registered with preference (fields directly associated with the programme): 0/80 - fields of study / plans the course is directly associated with
- there are 34 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: understand problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Sedimentary rocks:
- Rock-forming minerals of sedimentary rocks - origin and petrogenesis: clay minerals, silicon oxides and hydroxides, feldspars, carbonates, phosphates, oxides, Fe, Mn, Al-hydroxides, sulfates, chlorides, iron sulfides. Organic matters. Rock-forming organism.
- Origin and evolution of sedimentary structures: Textural characteristic (distribution of grain size, the shapes of sedimentary particles, surface texture of sedimentary particles, matrix, cements and cementation, ooids and pisoids, spherulitic texture, primary and secondary porosity, permeability). Textural classification. Structural classification of sedimentary rocks. Outer and inner structures.
- Origin of sedimentary rocks: weathering processes (mechanical and chemical degradation of rocks, sedimentary cycle, soil formation, erosion. Transport (medium motion, grain flows, water transport, eolian transport, glacial and gravitational processes, orientation of grains). Sedimentation, types of deposition environments. Influence of the tectonic and climatic conditions, sedimentation velocity. Maturity of sediments. Diagenesis of sediments, diagenetic evolution (syndiagenesis, anadiagenesis, epidiagenesis), main phases arising during lithogenesis, geophysical and geochemical conditions of diagenesis, Diagenetic metasomatism. Anchimetamorphism.
- Recent sediments.
- Metamorphic rocks
- Individual types of metamorphic rocks will be treated with emphasis on the geotectonic setting of their genesis. Methods of metamorphic rocks studies aiming at determination of P-T conditions of their formation will be presented. This will include analyses of relationships between metamorphism and deformation, formation and use of mineral zoning, geothermobarometry, geochronology, petrogenetic grids and metamorphic P-T paths. Examples from the Bohemian Massif will be presented.
- 1. Metapelites, quartzofeldspathic rocks (orthogneisses)
- 2. Metabasic and mafic rocks.
- 3. Metacarbonates, calc-silicate rocks .
- 4. High temperature and ultra-high temperature metamorphism, low, medium and high pressure granulites, anatexis, contact metamorphism.
- Literature
- HALL, Anthony. Igneous petrology. 2nd ed. Essex: Longman Group, 1996, xiv, 551. ISBN 0582230802. info
- MCLANE, Michael. Sedimentology. New York: Oxford University Press, 1995, xiii, 423. ISBN 0195078683. info
- BLATT, Harvey. Sedimentary petrology. 2nd ed. New York: W.H. Freeman, 1992, 514 s. ISBN 0-7167-2273-9. info
- KUKAL, Zdeněk. Základy sedimentologie. 1. vyd. Praha: Academia, 1986, 466 s. info
- KUKAL, Zdeněk. Geology of recent sediments. Praha: Academia, 1970, 490 s. info
- KONOPÁSEK, Jiří. Metamorfní petrologie. 1. vyd. Praha: Karolinum, 1998, 241 s. ISBN 8071846686. info
- Teaching methods
- lecture
- Assessment methods
- Lectures, written tests
- Language of instruction
- Czech
- Further comments (probably available only in Czech)
- Study Materials
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2010/2011.
G4021 Igneous and metamorphic petrology (II)
Faculty of ScienceAutumn 2008
- Extent and Intensity
- 2/0. 3 credit(s). Recommended Type of Completion: graded credit. Other types of completion: zk (examination).
- Teacher(s)
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat. (lecturer)
Mgr. David Buriánek, Ph.D. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer) - Guaranteed by
- doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr. - Timetable
- Mon 8:00–10:50 01006, Mon 11:00–11:50 01006
- Prerequisites
- ( G3021k Petrology I || G3021 Petrology I ) && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE4)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 11 student(s).
Current registration and enrolment status: enrolled: 0/11, only registered: 0/11, only registered with preference (fields directly associated with the programme): 0/11 - fields of study / plans the course is directly associated with
- there are 37 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: understand problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Sedimentary rocks:
- Rock-forming minerals of sedimentary rocks - origin and petrogenesis: clay minerals, silicon oxides and hydroxides, feldspars, carbonates, phosphates, oxides, Fe, Mn, Al-hydroxides, sulfates, chlorides, iron sulfides. Organic matters. Rock-forming organism.
- Origin and evolution of sedimentary structures: Textural characteristic (distribution of grain size, the shapes of sedimentary particles, surface texture of sedimentary particles, matrix, cements and cementation, ooids and pisoids, spherulitic texture, primary and secondary porosity, permeability). Textural classification. Structural classification of sedimentary rocks. Outer and inner structures.
- Origin of sedimentary rocks: weathering processes (mechanical and chemical degradation of rocks, sedimentary cycle, soil formation, erosion. Transport (medium motion, grain flows, water transport, eolian transport, glacial and gravitational processes, orientation of grains). Sedimentation, types of deposition environments. Influence of the tectonic and climatic conditions, sedimentation velocity. Maturity of sediments. Diagenesis of sediments, diagenetic evolution (syndiagenesis, anadiagenesis, epidiagenesis), main phases arising during lithogenesis, geophysical and geochemical conditions of diagenesis, Diagenetic metasomatism. Anchimetamorphism.
- Recent sediments.
- Metamorphic rocks
- Individual types of metamorphic rocks will be treated with emphasis on the geotectonic setting of their genesis. Methods of metamorphic rocks studies aiming at determination of P-T conditions of their formation will be presented. This will include analyses of relationships between metamorphism and deformation, formation and use of mineral zoning, geothermobarometry, geochronology, petrogenetic grids and metamorphic P-T paths. Examples from the Bohemian Massif will be presented.
- 1. Metapelites, quartzofeldspathic rocks (orthogneisses)
- 2. Metabasic and mafic rocks.
- 3. Metacarbonates, calc-silicate rocks .
- 4. High temperature and ultra-high temperature metamorphism, low, medium and high pressure granulites, anatexis, contact metamorphism.
- Literature
- HALL, Anthony. Igneous petrology. 2nd ed. Essex: Longman Group, 1996, xiv, 551. ISBN 0582230802. info
- MCLANE, Michael. Sedimentology. New York: Oxford University Press, 1995, xiii, 423. ISBN 0195078683. info
- BLATT, Harvey. Sedimentary petrology. 2nd ed. New York: W.H. Freeman, 1992, 514 s. ISBN 0-7167-2273-9. info
- KUKAL, Zdeněk. Základy sedimentologie. 1. vyd. Praha: Academia, 1986, 466 s. info
- KUKAL, Zdeněk. Geology of recent sediments. Praha: Academia, 1970, 490 s. info
- KONOPÁSEK, Jiří. Metamorfní petrologie. 1. vyd. Praha: Karolinum, 1998, 241 s. ISBN 8071846686. info
- Assessment methods
- Lectures, written tests
- Language of instruction
- Czech
- Further comments (probably available only in Czech)
- Study Materials
The course is taught once in two years.
Information on the per-term frequency of the course: Výuka proběhne v podzimním semestru akademického roku 2009/2010.
G4021 Petrology II
Faculty of ScienceAutumn 2007
- Extent and Intensity
- 3/1. 6 credit(s). Type of Completion: zk (examination).
- Teacher(s)
- doc. RNDr. Miroslava Gregerová, CSc. (lecturer)
doc. RNDr. Jana Kotková, CSc. (lecturer)
doc. RNDr. Jindřich Štelcl, CSc. (lecturer)
Mgr. David Buriánek, Ph.D. (lecturer)
Mgr. Lenka Dziková (seminar tutor) - Guaranteed by
- doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: Běla Hrbková - Timetable
- Wed 8:00–10:50 01006, Wed 15:00–17:50 01015b
- Prerequisites
- ( G3021 Petrology I || G3021k Petrology I ) && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Manipulation with chemicals )))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
- fields of study / plans the course is directly associated with
- there are 37 fields of study the course is directly associated with, display
- Course objectives
- This course is an extension of basic course - Petrology I. Subject deals with problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Sedimentary rocks:
- Rock-forming minerals of sedimentary rocks - origin and petrogenesis: clay minerals, silicon oxides and hydroxides, feldspars, carbonates, phosphates, oxides, Fe, Mn, Al-hydroxides, sulfates, chlorides, iron sulfides. Organic matters. Rock-forming organism.
- Origin and evolution of sedimentary structures: Textural characteristic (distribution of grain size, the shapes of sedimentary particles, surface texture of sedimentary particles, matrix, cements and cementation, ooids and pisoids, spherulitic texture, primary and secondary porosity, permeability). Textural classification. Structural classification of sedimentary rocks. Outer and inner structures.
- Origin of sedimentary rocks: weathering processes (mechanical and chemical degradation of rocks, sedimentary cycle, soil formation, erosion. Transport (medium motion, grain flows, water transport, eolian transport, glacial and gravitational processes, orientation of grains). Sedimentation, types of deposition environments. Influence of the tectonic and climatic conditions, sedimentation velocity. Maturity of sediments. Diagenesis of sediments, diagenetic evolution (syndiagenesis, anadiagenesis, epidiagenesis), main phases arising during lithogenesis, geophysical and geochemical conditions of diagenesis, Diagenetic metasomatism. Anchimetamorphism.
- Recent sediments.
- Metamorphic rocks
- Individual types of metamorphic rocks will be treated with emphasis on the geotectonic setting of their genesis. Methods of metamorphic rocks studies aiming at determination of P-T conditions of their formation will be presented. This will include analyses of relationships between metamorphism and deformation, formation and use of mineral zoning, geothermobarometry, geochronology, petrogenetic grids and metamorphic P-T paths. Examples from the Bohemian Massif will be presented.
- 1. Metapelites, quartzofeldspathic rocks (orthogneisses)
- 2. Metabasic and mafic rocks.
- 3. Metacarbonates, calc-silicate rocks .
- 4. High temperature and ultra-high temperature metamorphism, low, medium and high pressure granulites, anatexis, contact metamorphism.
- Literature
- HALL, Anthony. Igneous petrology. 2nd ed. Essex: Longman Group, 1996, xiv, 551. ISBN 0582230802. info
- MCLANE, Michael. Sedimentology. New York: Oxford University Press, 1995, xiii, 423. ISBN 0195078683. info
- BLATT, Harvey. Sedimentary petrology. 2nd ed. New York: W.H. Freeman, 1992, 514 s. ISBN 0-7167-2273-9. info
- KUKAL, Zdeněk. Základy sedimentologie. 1. vyd. Praha: Academia, 1986, 466 s. info
- KUKAL, Zdeněk. Geology of recent sediments. Praha: Academia, 1970, 490 s. info
- KONOPÁSEK, Jiří. Metamorfní petrologie. 1. vyd. Praha: Karolinum, 1998, 241 s. ISBN 8071846686. info
- Assessment methods (in Czech)
- Přednášky a praktická cvičení, každá skupina hornin (magmatické, metamorfované, sedimentární) bude ukončena testem. Ústní zkoušku mohou studenti vykonat pouze po úspěšném zvládnutí písemných části.
- Language of instruction
- Czech
- Further Comments
- Study Materials
The course is taught annually.
G4021 Petrology II
Faculty of ScienceAutumn 2006
- Extent and Intensity
- 3/1. 6 credit(s). Type of Completion: zk (examination).
- Teacher(s)
- doc. RNDr. Miroslava Gregerová, CSc. (lecturer)
doc. RNDr. Jana Kotková, CSc. (lecturer)
doc. RNDr. Jindřich Štelcl, CSc. (lecturer)
Mgr. David Buriánek, Ph.D. (lecturer) - Guaranteed by
- doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: Běla Hrbková - Timetable
- Wed 8:00–10:50 Bp1,01007
- Timetable of Seminar Groups:
G4021/02: Mon 16:00–16:50 01015b - Prerequisites
- G3021 Petrology I && (!( G4020 Sedimentary Petrology && G3020 Magmatic Petrology && G5100 Petrology of metamorphic rocks ))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 60 student(s).
Current registration and enrolment status: enrolled: 0/60, only registered: 0/60, only registered with preference (fields directly associated with the programme): 0/60 - fields of study / plans the course is directly associated with
- there are 37 fields of study the course is directly associated with, display
- Course objectives
- This course is an extension of basic course - Petrology I. Subject deals with problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Sedimentary rocks:
- Rock-forming minerals of sedimentary rocks - origin and petrogenesis: clay minerals, silicon oxides and hydroxides, feldspars, carbonates, phosphates, oxides, Fe, Mn, Al-hydroxides, sulfates, chlorides, iron sulfides. Organic matters. Rock-forming organism.
- Origin and evolution of sedimentary structures: Textural characteristic (distribution of grain size, the shapes of sedimentary particles, surface texture of sedimentary particles, matrix, cements and cementation, ooids and pisoids, spherulitic texture, primary and secondary porosity, permeability). Textural classification. Structural classification of sedimentary rocks. Outer and inner structures.
- Origin of sedimentary rocks: weathering processes (mechanical and chemical degradation of rocks, sedimentary cycle, soil formation, erosion. Transport (medium motion, grain flows, water transport, eolian transport, glacial and gravitational processes, orientation of grains). Sedimentation, types of deposition environments. Influence of the tectonic and climatic conditions, sedimentation velocity. Maturity of sediments. Diagenesis of sediments, diagenetic evolution (syndiagenesis, anadiagenesis, epidiagenesis), main phases arising during lithogenesis, geophysical and geochemical conditions of diagenesis, Diagenetic metasomatism. Anchimetamorphism.
- Recent sediments.
- Metamorphic rocks
- Individual types of metamorphic rocks will be treated with emphasis on the geotectonic setting of their genesis. Methods of metamorphic rocks studies aiming at determination of P-T conditions of their formation will be presented. This will include analyses of relationships between metamorphism and deformation, formation and use of mineral zoning, geothermobarometry, geochronology, petrogenetic grids and metamorphic P-T paths. Examples from the Bohemian Massif will be presented.
- 1. Metapelites, quartzofeldspathic rocks (orthogneisses)
- 2. Metabasic and mafic rocks.
- 3. Metacarbonates, calc-silicate rocks .
- 4. High temperature and ultra-high temperature metamorphism, low, medium and high pressure granulites, anatexis, contact metamorphism.
- Literature
- HALL, Anthony. Igneous petrology. 2nd ed. Essex: Longman Group, 1996, xiv, 551. ISBN 0582230802. info
- MCLANE, Michael. Sedimentology. New York: Oxford University Press, 1995, xiii, 423. ISBN 0195078683. info
- BLATT, Harvey. Sedimentary petrology. 2nd ed. New York: W.H. Freeman, 1992, 514 s. ISBN 0-7167-2273-9. info
- KUKAL, Zdeněk. Základy sedimentologie. 1. vyd. Praha: Academia, 1986, 466 s. info
- KUKAL, Zdeněk. Geology of recent sediments. Praha: Academia, 1970, 490 s. info
- KONOPÁSEK, Jiří. Metamorfní petrologie. 1. vyd. Praha: Karolinum, 1998, 241 s. ISBN 8071846686. info
- Assessment methods (in Czech)
- Přednášky a praktická cvičení, každá skupina hornin (magmatické, metamorfované, sedimentární) bude ukončena testem. Ústní zkoušku mohou studenti vykonat pouze po úspěšném zvládnutí písemných části.
- Language of instruction
- Czech
- Further Comments
- Study Materials
The course is taught annually.
G4021 Petrology II
Faculty of ScienceAutumn 2005
- Extent and Intensity
- 3/1. 4 credit(s) (fasci plus compl plus > 4). Type of Completion: zk (examination).
- Teacher(s)
- doc. RNDr. Miroslava Gregerová, CSc. (lecturer)
doc. RNDr. Jana Kotková, CSc. (lecturer)
doc. RNDr. Jindřich Štelcl, CSc. (lecturer)
Mgr. David Buriánek, Ph.D. (lecturer) - Guaranteed by
- doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: Běla Hrbková - Timetable
- Wed 7:00–9:50 G1,01004, Wed 10:00–10:50 G1,01004
- Prerequisites
- G3021 Petrology I && (!( G4020 Sedimentary Petrology && G3020 Magmatic Petrology && G5100 Petrology of metamorphic rocks ))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 60 student(s).
Current registration and enrolment status: enrolled: 0/60, only registered: 0/60, only registered with preference (fields directly associated with the programme): 0/60 - fields of study / plans the course is directly associated with
- there are 37 fields of study the course is directly associated with, display
- Course objectives
- This course is an extension of basic course - Petrology I. Subject deals with problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Sedimentary rocks:
- Rock-forming minerals of sedimentary rocks - origin and petrogenesis: clay minerals, silicon oxides and hydroxides, feldspars, carbonates, phosphates, oxides, Fe, Mn, Al-hydroxides, sulfates, chlorides, iron sulfides. Organic matters. Rock-forming organism.
- Origin and evolution of sedimentary structures: Textural characteristic (distribution of grain size, the shapes of sedimentary particles, surface texture of sedimentary particles, matrix, cements and cementation, ooids and pisoids, spherulitic texture, primary and secondary porosity, permeability). Textural classification. Structural classification of sedimentary rocks. Outer and inner structures.
- Origin of sedimentary rocks: weathering processes (mechanical and chemical degradation of rocks, sedimentary cycle, soil formation, erosion. Transport (medium motion, grain flows, water transport, eolian transport, glacial and gravitational processes, orientation of grains). Sedimentation, types of deposition environments. Influence of the tectonic and climatic conditions, sedimentation velocity. Maturity of sediments. Diagenesis of sediments, diagenetic evolution (syndiagenesis, anadiagenesis, epidiagenesis), main phases arising during lithogenesis, geophysical and geochemical conditions of diagenesis, Diagenetic metasomatism. Anchimetamorphism.
- Recent sediments.
- Metamorphic rocks
- Individual types of metamorphic rocks will be treated with emphasis on the geotectonic setting of their genesis. Methods of metamorphic rocks studies aiming at determination of P-T conditions of their formation will be presented. This will include analyses of relationships between metamorphism and deformation, formation and use of mineral zoning, geothermobarometry, geochronology, petrogenetic grids and metamorphic P-T paths. Examples from the Bohemian Massif will be presented.
- 1. Metapelites, quartzofeldspathic rocks (orthogneisses)
- 2. Metabasic and mafic rocks.
- 3. Metacarbonates, calc-silicate rocks .
- 4. High temperature and ultra-high temperature metamorphism, low, medium and high pressure granulites, anatexis, contact metamorphism.
- Literature
- HALL, Anthony. Igneous petrology. 2nd ed. Essex: Longman Group, 1996, xiv, 551. ISBN 0582230802. info
- MCLANE, Michael. Sedimentology. New York: Oxford University Press, 1995, xiii, 423. ISBN 0195078683. info
- BLATT, Harvey. Sedimentary petrology. 2nd ed. New York: W.H. Freeman, 1992, 514 s. ISBN 0-7167-2273-9. info
- KUKAL, Zdeněk. Základy sedimentologie. 1. vyd. Praha: Academia, 1986, 466 s. info
- KUKAL, Zdeněk. Geology of recent sediments. Praha: Academia, 1970, 490 s. info
- KONOPÁSEK, Jiří. Metamorfní petrologie. 1. vyd. Praha: Karolinum, 1998, 241 s. ISBN 8071846686. info
- Assessment methods (in Czech)
- Přednášky a praktická cvičení, každá skupina hornin (magmatické, metamorfované, sedimentární) bude ukončena testem. Ústní zkoušku mohou studenti vykonat pouze po úspěšném zvládnutí písemných části.
- Language of instruction
- Czech
- Further Comments
- Study Materials
The course is taught annually.
G4021 Petrology II
Faculty of ScienceAutumn 2004
- Extent and Intensity
- 3/1. 4 credit(s) (fasci plus compl plus > 4). Type of Completion: zk (examination).
- Teacher(s)
- doc. RNDr. Miroslava Gregerová, CSc. (lecturer)
doc. RNDr. Jana Kotková, CSc. (lecturer)
doc. RNDr. Jindřich Štelcl, CSc. (lecturer) - Guaranteed by
- doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: Běla Hrbková - Timetable
- Tue 7:00–9:50 G1,01004
- Timetable of Seminar Groups:
G4021/02: Wed 17:00–17:50 01015b - Prerequisites
- G3021 Petrology I && ((! G4020 Sedimentary Petrology ) && (! G3020 Magmatic Petrology ) && (! G5100 Petrology of metamorphic rocks ))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
- fields of study / plans the course is directly associated with
- Geology, Hydrogeology and Geochemistry (programme PřF, B-GE)
- Geology, Hydrogeology and Geochemistry (programme PřF, M-GE)
- Geology - Museology (programme PřF, B-GE)
- Course objectives
- This course is an extension of basic course - Petrology I. Subject deals with problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Sedimentary rocks:
- Rock-forming minerals of sedimentary rocks - origin and petrogenesis: clay minerals, silicon oxides and hydroxides, feldspars, carbonates, phosphates, oxides, Fe, Mn, Al-hydroxides, sulfates, chlorides, iron sulfides. Organic matters. Rock-forming organism.
- Origin and evolution of sedimentary structures: Textural characteristic (distribution of grain size, the shapes of sedimentary particles, surface texture of sedimentary particles, matrix, cements and cementation, ooids and pisoids, spherulitic texture, primary and secondary porosity, permeability). Textural classification. Structural classification of sedimentary rocks. Outer and inner structures.
- Origin of sedimentary rocks: weathering processes (mechanical and chemical degradation of rocks, sedimentary cycle, soil formation, erosion. Transport (medium motion, grain flows, water transport, eolian transport, glacial and gravitational processes, orientation of grains). Sedimentation, types of deposition environments. Influence of the tectonic and climatic conditions, sedimentation velocity. Maturity of sediments. Diagenesis of sediments, diagenetic evolution (syndiagenesis, anadiagenesis, epidiagenesis), main phases arising during lithogenesis, geophysical and geochemical conditions of diagenesis, Diagenetic metasomatism. Anchimetamorphism.
- Recent sediments.
- Metamorphic rocks
- Individual types of metamorphic rocks will be treated with emphasis on the geotectonic setting of their genesis. Methods of metamorphic rocks studies aiming at determination of P-T conditions of their formation will be presented. This will include analyses of relationships between metamorphism and deformation, formation and use of mineral zoning, geothermobarometry, geochronology, petrogenetic grids and metamorphic P-T paths. Examples from the Bohemian Massif will be presented.
- 1. Metapelites, quartzofeldspathic rocks (orthogneisses)
- 2. Metabasic and mafic rocks.
- 3. Metacarbonates, calc-silicate rocks .
- 4. High temperature and ultra-high temperature metamorphism, low, medium and high pressure granulites, anatexis, contact metamorphism.
- Literature
- HALL, Anthony. Igneous petrology. 2nd ed. Essex: Longman Group, 1996, xiv, 551. ISBN 0582230802. info
- MCLANE, Michael. Sedimentology. New York: Oxford University Press, 1995, xiii, 423. ISBN 0195078683. info
- BLATT, Harvey. Sedimentary petrology. 2nd ed. New York: W.H. Freeman, 1992, 514 s. ISBN 0-7167-2273-9. info
- KUKAL, Zdeněk. Základy sedimentologie. 1. vyd. Praha: Academia, 1986, 466 s. info
- KUKAL, Zdeněk. Geology of recent sediments. Praha: Academia, 1970, 490 s. info
- KONOPÁSEK, Jiří. Metamorfní petrologie. 1. vyd. Praha: Karolinum, 1998, 241 s. ISBN 8071846686. info
- Assessment methods (in Czech)
- Přednášky a praktická cvičení, každá skupina hornin (magmatické, metamorfované, sedimentární) bude ukončena testem. Ústní zkoušku mohou studenti vykonat pouze po úspěšném zvládnutí písemných části.
- Language of instruction
- Czech
- Further Comments
- The course is taught annually.
G4021 Petrology II
Faculty of ScienceAutumn 2003
- Extent and Intensity
- 3/1. 4 credit(s) (fasci plus compl plus > 4). Type of Completion: zk (examination).
- Teacher(s)
- doc. RNDr. Miroslava Gregerová, CSc. (lecturer)
doc. RNDr. Jana Kotková, CSc. (lecturer)
doc. RNDr. Jindřich Štelcl, CSc. (lecturer) - Guaranteed by
- doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: Běla Hrbková - Timetable of Seminar Groups
- G4021/1: No timetable has been entered into IS.
G4021/2: No timetable has been entered into IS. - Prerequisites
- G3021 Petrology I && ((! G4020 Sedimentary Petrology ) && (! G3020 Magmatic Petrology ) && (! G5100 Petrology of metamorphic rocks ))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 54 student(s).
Current registration and enrolment status: enrolled: 0/54, only registered: 0/54, only registered with preference (fields directly associated with the programme): 0/54 - fields of study / plans the course is directly associated with
- Geology, Hydrogeology and Geochemistry (programme PřF, B-GE)
- Geology, Hydrogeology and Geochemistry (programme PřF, M-GE)
- Geology - Museology (programme PřF, B-GE)
- Course objectives
- This course is an extension of basic course - Petrology I. Subject deals with problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Sedimentary rocks:
- Rock-forming minerals of sedimentary rocks - origin and petrogenesis: clay minerals, silicon oxides and hydroxides, feldspars, carbonates, phosphates, oxides, Fe, Mn, Al-hydroxides, sulfates, chlorides, iron sulfides. Organic matters. Rock-forming organism.
- Origin and evolution of sedimentary structures: Textural characteristic (distribution of grain size, the shapes of sedimentary particles, surface texture of sedimentary particles, matrix, cements and cementation, ooids and pisoids, spherulitic texture, primary and secondary porosity, permeability). Textural classification. Structural classification of sedimentary rocks. Outer and inner structures.
- Origin of sedimentary rocks: weathering processes (mechanical and chemical degradation of rocks, sedimentary cycle, soil formation, erosion. Transport (medium motion, grain flows, water transport, eolian transport, glacial and gravitational processes, orientation of grains). Sedimentation, types of deposition environments. Influence of the tectonic and climatic conditions, sedimentation velocity. Maturity of sediments. Diagenesis of sediments, diagenetic evolution (syndiagenesis, anadiagenesis, epidiagenesis), main phases arising during lithogenesis, geophysical and geochemical conditions of diagenesis, Diagenetic metasomatism. Anchimetamorphism.
- Recent sediments.
- Metamorphic rocks
- Individual types of metamorphic rocks will be treated with emphasis on the geotectonic setting of their genesis. Methods of metamorphic rocks studies aiming at determination of P-T conditions of their formation will be presented. This will include analyses of relationships between metamorphism and deformation, formation and use of mineral zoning, geothermobarometry, geochronology, petrogenetic grids and metamorphic P-T paths. Examples from the Bohemian Massif will be presented.
- 1. Metapelites, quartzofeldspathic rocks (orthogneisses)
- 2. Metabasic and mafic rocks.
- 3. Metacarbonates, calc-silicate rocks .
- 4. High temperature and ultra-high temperature metamorphism, low, medium and high pressure granulites, anatexis, contact metamorphism.
- Literature
- HALL, Anthony. Igneous petrology. 2nd ed. Essex: Longman Group, 1996, xiv, 551. ISBN 0582230802. info
- MCLANE, Michael. Sedimentology. New York: Oxford University Press, 1995, xiii, 423. ISBN 0195078683. info
- BLATT, Harvey. Sedimentary petrology. 2nd ed. New York: W.H. Freeman, 1992, 514 s. ISBN 0-7167-2273-9. info
- KUKAL, Zdeněk. Základy sedimentologie. 1. vyd. Praha: Academia, 1986, 466 s. info
- KUKAL, Zdeněk. Geology of recent sediments. Praha: Academia, 1970, 490 s. info
- KONOPÁSEK, Jiří. Metamorfní petrologie. 1. vyd. Praha: Karolinum, 1998, 241 s. ISBN 8071846686. info
- Assessment methods (in Czech)
- Přednášky a praktická cvičení, každá skupina hornin (magmatické, metamorfované, sedimentární) bude ukončena testem. Ústní zkoušku mohou studenti vykonat pouze po úspěšném zvládnutí písemných části.
- Language of instruction
- Czech
- Further Comments
- The course is taught annually.
G4021 Petrology II
Faculty of ScienceAutumn 2002
- Extent and Intensity
- 3/1. 4 credit(s) (fasci plus compl plus > 4). Type of Completion: zk (examination).
- Teacher(s)
- doc. RNDr. Miroslava Gregerová, CSc. (lecturer)
doc. RNDr. Jana Kotková, CSc. (lecturer)
doc. RNDr. Jindřich Štelcl, CSc. (lecturer) - Guaranteed by
- doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. RNDr. Jindřich Štelcl, CSc. - Prerequisites
- G3021 Petrology I && ((! G4020 Sedimentary Petrology ) && (! G3020 Magmatic Petrology ) && (! G5100 Petrology of metamorphic rocks ))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
- fields of study / plans the course is directly associated with
- Geology, Hydrogeology and Geochemistry (programme PřF, B-GE)
- Geology, Hydrogeology and Geochemistry (programme PřF, M-GE)
- Geology - Museology (programme PřF, B-GE)
- Course objectives
- This course is an extension of basic course - Petrology I. Subject deals with problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Sedimentary rocks:
- Rock-forming minerals of sedimentary rocks - origin and petrogenesis: clay minerals, silicon oxides and hydroxides, feldspars, carbonates, phosphates, oxides, Fe, Mn, Al-hydroxides, sulfates, chlorides, iron sulfides. Organic matters. Rock-forming organism.
- Origin and evolution of sedimentary structures: Textural characteristic (distribution of grain size, the shapes of sedimentary particles, surface texture of sedimentary particles, matrix, cements and cementation, ooids and pisoids, spherulitic texture, primary and secondary porosity, permeability). Textural classification. Structural classification of sedimentary rocks. Outer and inner structures.
- Origin of sedimentary rocks: weathering processes (mechanical and chemical degradation of rocks, sedimentary cycle, soil formation, erosion. Transport (medium motion, grain flows, water transport, eolian transport, glacial and gravitational processes, orientation of grains). Sedimentation, types of deposition environments. Influence of the tectonic and climatic conditions, sedimentation velocity. Maturity of sediments. Diagenesis of sediments, diagenetic evolution (syndiagenesis, anadiagenesis, epidiagenesis), main phases arising during lithogenesis, geophysical and geochemical conditions of diagenesis, Diagenetic metasomatism. Anchimetamorphism.
- Recent sediments.
- Metamorphic rocks
- Individual types of metamorphic rocks will be treated with emphasis on the geotectonic setting of their genesis. Methods of metamorphic rocks studies aiming at determination of P-T conditions of their formation will be presented. This will include analyses of relationships between metamorphism and deformation, formation and use of mineral zoning, geothermobarometry, geochronology, petrogenetic grids and metamorphic P-T paths. Examples from the Bohemian Massif will be presented.
- 1. Metapelites, quartzofeldspathic rocks (orthogneisses)
- 2. Metabasic and mafic rocks.
- 3. Metacarbonates, calc-silicate rocks .
- 4. High temperature and ultra-high temperature metamorphism, low, medium and high pressure granulites, anatexis, contact metamorphism.
- Literature
- HALL, Anthony. Igneous petrology. 2nd ed. Essex: Longman Group, 1996, xiv, 551. ISBN 0582230802. info
- MCLANE, Michael. Sedimentology. New York: Oxford University Press, 1995, xiii, 423. ISBN 0195078683. info
- BLATT, Harvey. Sedimentary petrology. 2nd ed. New York: W.H. Freeman, 1992, 514 s. ISBN 0-7167-2273-9. info
- KUKAL, Zdeněk. Základy sedimentologie. 1. vyd. Praha: Academia, 1986, 466 s. info
- KUKAL, Zdeněk. Geology of recent sediments. Praha: Academia, 1970, 490 s. info
- KONOPÁSEK, Jiří. Metamorfní petrologie. 1. vyd. Praha: Karolinum, 1998, 241 s. ISBN 8071846686. info
- Assessment methods (in Czech)
- Přednášky a praktická cvičení, každá skupina hornin (magmatické, metamorfované, sedimentární) bude ukončena testem. Ústní zkoušku mohou studenti vykonat pouze po úspěšném zvládnutí písemných části.
- Language of instruction
- Czech
- Further Comments
- The course is taught annually.
The course is taught: every week.
G4021 Igneous petrology
Faculty of ScienceAutumn 2023
The course is not taught in Autumn 2023
- Extent and Intensity
- 2/1/0. 5 credit(s). Type of Completion: zk (examination).
- Teacher(s)
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat. (lecturer)
Petra Ludvová Hašková, DiS. (assistant) - Guaranteed by
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: Ing. Jana Pechmannová
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science - Prerequisites
- (PROGRAM(KOS)|| G3021k Petrography || G3021 Petrography ) && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE4)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemical substances )))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 78 student(s).
Current registration and enrolment status: enrolled: 0/78, only registered: 0/78, only registered with preference (fields directly associated with the programme): 0/78 - fields of study / plans the course is directly associated with
- there are 32 fields of study the course is directly associated with, display
- Course objectives
- The course aims to the genesis of the most important rock groups.
- Learning outcomes
- At the end of this course, students should be able to: understand problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Literature
- HALL, Anthony. Igneous petrology. 2nd ed. Essex: Longman Group, 1996, xiv, 551. ISBN 0582230802. info
- WINTER, John D. An introduction to igneous and metamorphic petrology. 2nd ed. Upper Saddle River, N.J.: Prentice Hall, 2010, xviii, 702. ISBN 9780321592576. info
- BEST, Myron G. Igneous petrology. Malden, Massachusetts: Blackwell Science, 2001, xvi, 458 s. ISBN 0-86542-541-8. info
- KONOPÁSEK, Jiří. Metamorfní petrologie. 1. vyd. Praha: Karolinum, 1998, 241 s. ISBN 8071846686. info
- MCLANE, Michael. Sedimentology. New York: Oxford University Press, 1995, xiii, 423. ISBN 0195078683. info
- BLATT, Harvey. Sedimentary petrology. 2nd ed. New York: W.H. Freeman, 1992, 514 s. ISBN 0716722739. info
- Teaching methods
- lecture
- Assessment methods
- Lectures, written tests
- Language of instruction
- Czech
- Further comments (probably available only in Czech)
- The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2022/2023.
The course is taught: every week.
G4021 Igneous petrology
Faculty of Scienceautumn 2021
The course is not taught in autumn 2021
- Extent and Intensity
- 2/1/0. 5 credit(s). Type of Completion: zk (examination).
- Teacher(s)
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat. (lecturer)
Petra Ludvová Hašková, DiS. (assistant) - Guaranteed by
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science - Prerequisites
- (PROGRAM(KOS)|| G3021k Petrography || G3021 Petrography ) && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE4)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemical substances )))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 78 student(s).
Current registration and enrolment status: enrolled: 0/78, only registered: 0/78, only registered with preference (fields directly associated with the programme): 0/78 - fields of study / plans the course is directly associated with
- there are 32 fields of study the course is directly associated with, display
- Course objectives
- The course aims to the genesis of the most important rock groups.
- Learning outcomes
- At the end of this course, students should be able to: understand problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Literature
- HALL, Anthony. Igneous petrology. 2nd ed. Essex: Longman Group, 1996, xiv, 551. ISBN 0582230802. info
- WINTER, John D. An introduction to igneous and metamorphic petrology. 2nd ed. Upper Saddle River, N.J.: Prentice Hall, 2010, xviii, 702. ISBN 9780321592576. info
- BEST, Myron G. Igneous petrology. Malden, Massachusetts: Blackwell Science, 2001, xvi, 458 s. ISBN 0-86542-541-8. info
- KONOPÁSEK, Jiří. Metamorfní petrologie. 1. vyd. Praha: Karolinum, 1998, 241 s. ISBN 8071846686. info
- MCLANE, Michael. Sedimentology. New York: Oxford University Press, 1995, xiii, 423. ISBN 0195078683. info
- BLATT, Harvey. Sedimentary petrology. 2nd ed. New York: W.H. Freeman, 1992, 514 s. ISBN 0716722739. info
- Teaching methods
- lecture
- Assessment methods
- Lectures, written tests
- Language of instruction
- Czech
- Further comments (probably available only in Czech)
- The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2022/2023.
The course is taught: every week.
G4021 Igneous petrology
Faculty of ScienceAutumn 2019
The course is not taught in Autumn 2019
- Extent and Intensity
- 2/1/0. 5 credit(s). Type of Completion: zk (examination).
- Teacher(s)
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat. (lecturer)
- Guaranteed by
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science - Prerequisites
- (PROGRAM(KOS)|| G3021k Petrography || G3021 Petrography ) && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE4)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 78 student(s).
Current registration and enrolment status: enrolled: 0/78, only registered: 0/78, only registered with preference (fields directly associated with the programme): 0/78 - fields of study / plans the course is directly associated with
- there are 32 fields of study the course is directly associated with, display
- Course objectives
- The course aims to the genesis of the most important rock groups.
- Learning outcomes
- At the end of this course, students should be able to: understand problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Literature
- Teaching methods
- lecture
- Assessment methods
- Lectures, written tests
- Language of instruction
- Czech
- Further comments (probably available only in Czech)
- The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2020/2021.
The course is taught: every week.
G4021 Igneous and metamorphic petrology (II)
Faculty of Scienceautumn 2017
The course is not taught in autumn 2017
- Extent and Intensity
- 2/0. 3 credit(s). Type of Completion: graded credit.
- Teacher(s)
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat. (lecturer)
Mgr. David Buriánek, Ph.D. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Mgr. Vojtěch Wertich, Ph.D. (seminar tutor) - Guaranteed by
- doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science - Prerequisites
- (PROGRAM(KOS)|| G3021k Petrology I || G3021 Petrology I ) && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE4)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 80 student(s).
Current registration and enrolment status: enrolled: 0/80, only registered: 0/80, only registered with preference (fields directly associated with the programme): 0/80 - fields of study / plans the course is directly associated with
- there are 14 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: understand problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Sedimentary rocks:
- Rock-forming minerals of sedimentary rocks - origin and petrogenesis: clay minerals, silicon oxides and hydroxides, feldspars, carbonates, phosphates, oxides, Fe, Mn, Al-hydroxides, sulfates, chlorides, iron sulfides. Organic matters. Rock-forming organism.
- Origin and evolution of sedimentary structures: Textural characteristic (distribution of grain size, the shapes of sedimentary particles, surface texture of sedimentary particles, matrix, cements and cementation, ooids and pisoids, spherulitic texture, primary and secondary porosity, permeability). Textural classification. Structural classification of sedimentary rocks. Outer and inner structures.
- Origin of sedimentary rocks: weathering processes (mechanical and chemical degradation of rocks, sedimentary cycle, soil formation, erosion. Transport (medium motion, grain flows, water transport, eolian transport, glacial and gravitational processes, orientation of grains). Sedimentation, types of deposition environments. Influence of the tectonic and climatic conditions, sedimentation velocity. Maturity of sediments. Diagenesis of sediments, diagenetic evolution (syndiagenesis, anadiagenesis, epidiagenesis), main phases arising during lithogenesis, geophysical and geochemical conditions of diagenesis, Diagenetic metasomatism. Anchimetamorphism.
- Recent sediments.
- Metamorphic rocks
- Individual types of metamorphic rocks will be treated with emphasis on the geotectonic setting of their genesis. Methods of metamorphic rocks studies aiming at determination of P-T conditions of their formation will be presented. This will include analyses of relationships between metamorphism and deformation, formation and use of mineral zoning, geothermobarometry, geochronology, petrogenetic grids and metamorphic P-T paths. Examples from the Bohemian Massif will be presented.
- 1. Metapelites, quartzofeldspathic rocks (orthogneisses)
- 2. Metabasic and mafic rocks.
- 3. Metacarbonates, calc-silicate rocks .
- 4. High temperature and ultra-high temperature metamorphism, low, medium and high pressure granulites, anatexis, contact metamorphism.
- Literature
- HALL, Anthony. Igneous petrology. 2nd ed. Essex: Longman Group, 1996, xiv, 551. ISBN 0582230802. info
- MCLANE, Michael. Sedimentology. New York: Oxford University Press, 1995, xiii, 423. ISBN 0195078683. info
- BLATT, Harvey. Sedimentary petrology. 2nd ed. New York: W.H. Freeman, 1992, 514 s. ISBN 0-7167-2273-9. info
- KUKAL, Zdeněk. Základy sedimentologie. 1. vyd. Praha: Academia, 1986, 466 s. info
- KUKAL, Zdeněk. Geology of recent sediments. Praha: Academia, 1970, 490 s. info
- KONOPÁSEK, Jiří. Metamorfní petrologie. 1. vyd. Praha: Karolinum, 1998, 241 s. ISBN 8071846686. info
- BEST, Myron G. Igneous petrology. Malden, Massachusetts: Blackwell Science, 2001, xvi, 458 s. ISBN 0-86542-541-8. info
- Teaching methods
- lecture
- Assessment methods
- Lectures, written tests
- Language of instruction
- Czech
- Further comments (probably available only in Czech)
- The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2018/2019.
The course is taught: every week.
G4021 Igneous and metamorphic petrology (II)
Faculty of ScienceAutumn 2015
The course is not taught in Autumn 2015
- Extent and Intensity
- 2/0. 3 credit(s). Type of Completion: graded credit.
- Teacher(s)
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat. (lecturer)
Mgr. David Buriánek, Ph.D. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Mgr. Vojtěch Wertich, Ph.D. (seminar tutor) - Guaranteed by
- doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science - Prerequisites
- ( G3021k Petrology I || G3021 Petrology I ) && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE4)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 150 student(s).
Current registration and enrolment status: enrolled: 0/150, only registered: 0/150, only registered with preference (fields directly associated with the programme): 0/150 - fields of study / plans the course is directly associated with
- there are 14 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: understand problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Sedimentary rocks:
- Rock-forming minerals of sedimentary rocks - origin and petrogenesis: clay minerals, silicon oxides and hydroxides, feldspars, carbonates, phosphates, oxides, Fe, Mn, Al-hydroxides, sulfates, chlorides, iron sulfides. Organic matters. Rock-forming organism.
- Origin and evolution of sedimentary structures: Textural characteristic (distribution of grain size, the shapes of sedimentary particles, surface texture of sedimentary particles, matrix, cements and cementation, ooids and pisoids, spherulitic texture, primary and secondary porosity, permeability). Textural classification. Structural classification of sedimentary rocks. Outer and inner structures.
- Origin of sedimentary rocks: weathering processes (mechanical and chemical degradation of rocks, sedimentary cycle, soil formation, erosion. Transport (medium motion, grain flows, water transport, eolian transport, glacial and gravitational processes, orientation of grains). Sedimentation, types of deposition environments. Influence of the tectonic and climatic conditions, sedimentation velocity. Maturity of sediments. Diagenesis of sediments, diagenetic evolution (syndiagenesis, anadiagenesis, epidiagenesis), main phases arising during lithogenesis, geophysical and geochemical conditions of diagenesis, Diagenetic metasomatism. Anchimetamorphism.
- Recent sediments.
- Metamorphic rocks
- Individual types of metamorphic rocks will be treated with emphasis on the geotectonic setting of their genesis. Methods of metamorphic rocks studies aiming at determination of P-T conditions of their formation will be presented. This will include analyses of relationships between metamorphism and deformation, formation and use of mineral zoning, geothermobarometry, geochronology, petrogenetic grids and metamorphic P-T paths. Examples from the Bohemian Massif will be presented.
- 1. Metapelites, quartzofeldspathic rocks (orthogneisses)
- 2. Metabasic and mafic rocks.
- 3. Metacarbonates, calc-silicate rocks .
- 4. High temperature and ultra-high temperature metamorphism, low, medium and high pressure granulites, anatexis, contact metamorphism.
- Literature
- HALL, Anthony. Igneous petrology. 2nd ed. Essex: Longman Group, 1996, xiv, 551. ISBN 0582230802. info
- MCLANE, Michael. Sedimentology. New York: Oxford University Press, 1995, xiii, 423. ISBN 0195078683. info
- BLATT, Harvey. Sedimentary petrology. 2nd ed. New York: W.H. Freeman, 1992, 514 s. ISBN 0-7167-2273-9. info
- KUKAL, Zdeněk. Základy sedimentologie. 1. vyd. Praha: Academia, 1986, 466 s. info
- KUKAL, Zdeněk. Geology of recent sediments. Praha: Academia, 1970, 490 s. info
- KONOPÁSEK, Jiří. Metamorfní petrologie. 1. vyd. Praha: Karolinum, 1998, 241 s. ISBN 8071846686. info
- BEST, Myron G. Igneous petrology. Malden, Massachusetts: Blackwell Science, 2001, xvi, 458 s. ISBN 0-86542-541-8. info
- Teaching methods
- lecture
- Assessment methods
- Lectures, written tests
- Language of instruction
- Czech
- Further comments (probably available only in Czech)
- The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2014/2015.
The course is taught: every week.
G4021 Igneous and metamorphic petrology (II)
Faculty of ScienceAutumn 2013
The course is not taught in Autumn 2013
- Extent and Intensity
- 2/0. 3 credit(s). Type of Completion: graded credit.
- Teacher(s)
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat. (lecturer)
Mgr. David Buriánek, Ph.D. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer) - Guaranteed by
- doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science - Prerequisites
- ( G3021k Petrology I || G3021 Petrology I ) && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE4)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 150 student(s).
Current registration and enrolment status: enrolled: 0/150, only registered: 0/150, only registered with preference (fields directly associated with the programme): 0/150 - fields of study / plans the course is directly associated with
- there are 14 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: understand problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Sedimentary rocks:
- Rock-forming minerals of sedimentary rocks - origin and petrogenesis: clay minerals, silicon oxides and hydroxides, feldspars, carbonates, phosphates, oxides, Fe, Mn, Al-hydroxides, sulfates, chlorides, iron sulfides. Organic matters. Rock-forming organism.
- Origin and evolution of sedimentary structures: Textural characteristic (distribution of grain size, the shapes of sedimentary particles, surface texture of sedimentary particles, matrix, cements and cementation, ooids and pisoids, spherulitic texture, primary and secondary porosity, permeability). Textural classification. Structural classification of sedimentary rocks. Outer and inner structures.
- Origin of sedimentary rocks: weathering processes (mechanical and chemical degradation of rocks, sedimentary cycle, soil formation, erosion. Transport (medium motion, grain flows, water transport, eolian transport, glacial and gravitational processes, orientation of grains). Sedimentation, types of deposition environments. Influence of the tectonic and climatic conditions, sedimentation velocity. Maturity of sediments. Diagenesis of sediments, diagenetic evolution (syndiagenesis, anadiagenesis, epidiagenesis), main phases arising during lithogenesis, geophysical and geochemical conditions of diagenesis, Diagenetic metasomatism. Anchimetamorphism.
- Recent sediments.
- Metamorphic rocks
- Individual types of metamorphic rocks will be treated with emphasis on the geotectonic setting of their genesis. Methods of metamorphic rocks studies aiming at determination of P-T conditions of their formation will be presented. This will include analyses of relationships between metamorphism and deformation, formation and use of mineral zoning, geothermobarometry, geochronology, petrogenetic grids and metamorphic P-T paths. Examples from the Bohemian Massif will be presented.
- 1. Metapelites, quartzofeldspathic rocks (orthogneisses)
- 2. Metabasic and mafic rocks.
- 3. Metacarbonates, calc-silicate rocks .
- 4. High temperature and ultra-high temperature metamorphism, low, medium and high pressure granulites, anatexis, contact metamorphism.
- Literature
- Teaching methods
- lecture
- Assessment methods
- Lectures, written tests
- Language of instruction
- Czech
- Further comments (probably available only in Czech)
- The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2014/2015.
The course is taught: every week.
G4021 Igneous and metamorphic petrology (II)
Faculty of ScienceAutumn 2011
The course is not taught in Autumn 2011
- Extent and Intensity
- 2/0. 3 credit(s). Type of Completion: graded credit.
- Teacher(s)
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat. (lecturer)
Mgr. David Buriánek, Ph.D. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer) - Guaranteed by
- doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr. - Prerequisites
- ( G3021k Petrology I || G3021 Petrology I ) && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE4)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 1 student(s).
Current registration and enrolment status: enrolled: 0/1, only registered: 0/1, only registered with preference (fields directly associated with the programme): 0/1 - fields of study / plans the course is directly associated with
- there are 34 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: understand problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Sedimentary rocks:
- Rock-forming minerals of sedimentary rocks - origin and petrogenesis: clay minerals, silicon oxides and hydroxides, feldspars, carbonates, phosphates, oxides, Fe, Mn, Al-hydroxides, sulfates, chlorides, iron sulfides. Organic matters. Rock-forming organism.
- Origin and evolution of sedimentary structures: Textural characteristic (distribution of grain size, the shapes of sedimentary particles, surface texture of sedimentary particles, matrix, cements and cementation, ooids and pisoids, spherulitic texture, primary and secondary porosity, permeability). Textural classification. Structural classification of sedimentary rocks. Outer and inner structures.
- Origin of sedimentary rocks: weathering processes (mechanical and chemical degradation of rocks, sedimentary cycle, soil formation, erosion. Transport (medium motion, grain flows, water transport, eolian transport, glacial and gravitational processes, orientation of grains). Sedimentation, types of deposition environments. Influence of the tectonic and climatic conditions, sedimentation velocity. Maturity of sediments. Diagenesis of sediments, diagenetic evolution (syndiagenesis, anadiagenesis, epidiagenesis), main phases arising during lithogenesis, geophysical and geochemical conditions of diagenesis, Diagenetic metasomatism. Anchimetamorphism.
- Recent sediments.
- Metamorphic rocks
- Individual types of metamorphic rocks will be treated with emphasis on the geotectonic setting of their genesis. Methods of metamorphic rocks studies aiming at determination of P-T conditions of their formation will be presented. This will include analyses of relationships between metamorphism and deformation, formation and use of mineral zoning, geothermobarometry, geochronology, petrogenetic grids and metamorphic P-T paths. Examples from the Bohemian Massif will be presented.
- 1. Metapelites, quartzofeldspathic rocks (orthogneisses)
- 2. Metabasic and mafic rocks.
- 3. Metacarbonates, calc-silicate rocks .
- 4. High temperature and ultra-high temperature metamorphism, low, medium and high pressure granulites, anatexis, contact metamorphism.
- Literature
- HALL, Anthony. Igneous petrology. 2nd ed. Essex: Longman Group, 1996, xiv, 551. ISBN 0582230802. info
- MCLANE, Michael. Sedimentology. New York: Oxford University Press, 1995, xiii, 423. ISBN 0195078683. info
- BLATT, Harvey. Sedimentary petrology. 2nd ed. New York: W.H. Freeman, 1992, 514 s. ISBN 0-7167-2273-9. info
- KUKAL, Zdeněk. Základy sedimentologie. 1. vyd. Praha: Academia, 1986, 466 s. info
- KUKAL, Zdeněk. Geology of recent sediments. Praha: Academia, 1970, 490 s. info
- KONOPÁSEK, Jiří. Metamorfní petrologie. 1. vyd. Praha: Karolinum, 1998, 241 s. ISBN 8071846686. info
- Teaching methods
- lecture
- Assessment methods
- Lectures, written tests
- Language of instruction
- Czech
- Further comments (probably available only in Czech)
- The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2012/2013.
The course is taught: every week.
G4021 Igneous and metamorphic petrology (II)
Faculty of ScienceAutumn 2009
The course is not taught in Autumn 2009
- Extent and Intensity
- 2/0. 3 credit(s). Recommended Type of Completion: graded credit. Other types of completion: zk (examination).
- Teacher(s)
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat. (lecturer)
Mgr. David Buriánek, Ph.D. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer) - Guaranteed by
- doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr. - Prerequisites
- ( G3021k Petrology I || G3021 Petrology I ) && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE4)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
- fields of study / plans the course is directly associated with
- there are 37 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: understand problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Sedimentary rocks:
- Rock-forming minerals of sedimentary rocks - origin and petrogenesis: clay minerals, silicon oxides and hydroxides, feldspars, carbonates, phosphates, oxides, Fe, Mn, Al-hydroxides, sulfates, chlorides, iron sulfides. Organic matters. Rock-forming organism.
- Origin and evolution of sedimentary structures: Textural characteristic (distribution of grain size, the shapes of sedimentary particles, surface texture of sedimentary particles, matrix, cements and cementation, ooids and pisoids, spherulitic texture, primary and secondary porosity, permeability). Textural classification. Structural classification of sedimentary rocks. Outer and inner structures.
- Origin of sedimentary rocks: weathering processes (mechanical and chemical degradation of rocks, sedimentary cycle, soil formation, erosion. Transport (medium motion, grain flows, water transport, eolian transport, glacial and gravitational processes, orientation of grains). Sedimentation, types of deposition environments. Influence of the tectonic and climatic conditions, sedimentation velocity. Maturity of sediments. Diagenesis of sediments, diagenetic evolution (syndiagenesis, anadiagenesis, epidiagenesis), main phases arising during lithogenesis, geophysical and geochemical conditions of diagenesis, Diagenetic metasomatism. Anchimetamorphism.
- Recent sediments.
- Metamorphic rocks
- Individual types of metamorphic rocks will be treated with emphasis on the geotectonic setting of their genesis. Methods of metamorphic rocks studies aiming at determination of P-T conditions of their formation will be presented. This will include analyses of relationships between metamorphism and deformation, formation and use of mineral zoning, geothermobarometry, geochronology, petrogenetic grids and metamorphic P-T paths. Examples from the Bohemian Massif will be presented.
- 1. Metapelites, quartzofeldspathic rocks (orthogneisses)
- 2. Metabasic and mafic rocks.
- 3. Metacarbonates, calc-silicate rocks .
- 4. High temperature and ultra-high temperature metamorphism, low, medium and high pressure granulites, anatexis, contact metamorphism.
- Literature
- HALL, Anthony. Igneous petrology. 2nd ed. Essex: Longman Group, 1996, xiv, 551. ISBN 0582230802. info
- MCLANE, Michael. Sedimentology. New York: Oxford University Press, 1995, xiii, 423. ISBN 0195078683. info
- BLATT, Harvey. Sedimentary petrology. 2nd ed. New York: W.H. Freeman, 1992, 514 s. ISBN 0-7167-2273-9. info
- KUKAL, Zdeněk. Základy sedimentologie. 1. vyd. Praha: Academia, 1986, 466 s. info
- KUKAL, Zdeněk. Geology of recent sediments. Praha: Academia, 1970, 490 s. info
- KONOPÁSEK, Jiří. Metamorfní petrologie. 1. vyd. Praha: Karolinum, 1998, 241 s. ISBN 8071846686. info
- Teaching methods
- lecture
- Assessment methods
- Lectures, written tests
- Language of instruction
- Czech
- Further comments (probably available only in Czech)
- The course is taught once in two years.
Information on the per-term frequency of the course: Výuka proběhne v podzimním semestru akademického roku 2010/2011.
The course is taught: every week.
G4021 Igneous and metamorphic petrology (II)
Faculty of ScienceAutumn 2011 - acreditation
The information about the term Autumn 2011 - acreditation is not made public
- Extent and Intensity
- 2/0. 3 credit(s). Type of Completion: graded credit.
- Teacher(s)
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat. (lecturer)
Mgr. David Buriánek, Ph.D. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer) - Guaranteed by
- doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr. - Prerequisites
- ( G3021k Petrology I || G3021 Petrology I ) && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE4)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 80 student(s).
Current registration and enrolment status: enrolled: 0/80, only registered: 0/80, only registered with preference (fields directly associated with the programme): 0/80 - fields of study / plans the course is directly associated with
- there are 34 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: understand problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Sedimentary rocks:
- Rock-forming minerals of sedimentary rocks - origin and petrogenesis: clay minerals, silicon oxides and hydroxides, feldspars, carbonates, phosphates, oxides, Fe, Mn, Al-hydroxides, sulfates, chlorides, iron sulfides. Organic matters. Rock-forming organism.
- Origin and evolution of sedimentary structures: Textural characteristic (distribution of grain size, the shapes of sedimentary particles, surface texture of sedimentary particles, matrix, cements and cementation, ooids and pisoids, spherulitic texture, primary and secondary porosity, permeability). Textural classification. Structural classification of sedimentary rocks. Outer and inner structures.
- Origin of sedimentary rocks: weathering processes (mechanical and chemical degradation of rocks, sedimentary cycle, soil formation, erosion. Transport (medium motion, grain flows, water transport, eolian transport, glacial and gravitational processes, orientation of grains). Sedimentation, types of deposition environments. Influence of the tectonic and climatic conditions, sedimentation velocity. Maturity of sediments. Diagenesis of sediments, diagenetic evolution (syndiagenesis, anadiagenesis, epidiagenesis), main phases arising during lithogenesis, geophysical and geochemical conditions of diagenesis, Diagenetic metasomatism. Anchimetamorphism.
- Recent sediments.
- Metamorphic rocks
- Individual types of metamorphic rocks will be treated with emphasis on the geotectonic setting of their genesis. Methods of metamorphic rocks studies aiming at determination of P-T conditions of their formation will be presented. This will include analyses of relationships between metamorphism and deformation, formation and use of mineral zoning, geothermobarometry, geochronology, petrogenetic grids and metamorphic P-T paths. Examples from the Bohemian Massif will be presented.
- 1. Metapelites, quartzofeldspathic rocks (orthogneisses)
- 2. Metabasic and mafic rocks.
- 3. Metacarbonates, calc-silicate rocks .
- 4. High temperature and ultra-high temperature metamorphism, low, medium and high pressure granulites, anatexis, contact metamorphism.
- Literature
- Teaching methods
- lecture
- Assessment methods
- Lectures, written tests
- Language of instruction
- Czech
- Further comments (probably available only in Czech)
- Study Materials
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2010/2011.
The course is taught: every week.
G4021 Igneous and metamorphic petrology (II)
Faculty of ScienceAutumn 2010 - only for the accreditation
- Extent and Intensity
- 2/0. 3 credit(s). Type of Completion: graded credit.
- Teacher(s)
- prof. RNDr. Jaromír Leichmann, Dr. rer. nat. (lecturer)
Mgr. David Buriánek, Ph.D. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer) - Guaranteed by
- doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr. - Prerequisites
- ( G3021k Petrology I || G3021 Petrology I ) && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE4)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 80 student(s).
Current registration and enrolment status: enrolled: 0/80, only registered: 0/80, only registered with preference (fields directly associated with the programme): 0/80 - fields of study / plans the course is directly associated with
- there are 34 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: understand problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Sedimentary rocks:
- Rock-forming minerals of sedimentary rocks - origin and petrogenesis: clay minerals, silicon oxides and hydroxides, feldspars, carbonates, phosphates, oxides, Fe, Mn, Al-hydroxides, sulfates, chlorides, iron sulfides. Organic matters. Rock-forming organism.
- Origin and evolution of sedimentary structures: Textural characteristic (distribution of grain size, the shapes of sedimentary particles, surface texture of sedimentary particles, matrix, cements and cementation, ooids and pisoids, spherulitic texture, primary and secondary porosity, permeability). Textural classification. Structural classification of sedimentary rocks. Outer and inner structures.
- Origin of sedimentary rocks: weathering processes (mechanical and chemical degradation of rocks, sedimentary cycle, soil formation, erosion. Transport (medium motion, grain flows, water transport, eolian transport, glacial and gravitational processes, orientation of grains). Sedimentation, types of deposition environments. Influence of the tectonic and climatic conditions, sedimentation velocity. Maturity of sediments. Diagenesis of sediments, diagenetic evolution (syndiagenesis, anadiagenesis, epidiagenesis), main phases arising during lithogenesis, geophysical and geochemical conditions of diagenesis, Diagenetic metasomatism. Anchimetamorphism.
- Recent sediments.
- Metamorphic rocks
- Individual types of metamorphic rocks will be treated with emphasis on the geotectonic setting of their genesis. Methods of metamorphic rocks studies aiming at determination of P-T conditions of their formation will be presented. This will include analyses of relationships between metamorphism and deformation, formation and use of mineral zoning, geothermobarometry, geochronology, petrogenetic grids and metamorphic P-T paths. Examples from the Bohemian Massif will be presented.
- 1. Metapelites, quartzofeldspathic rocks (orthogneisses)
- 2. Metabasic and mafic rocks.
- 3. Metacarbonates, calc-silicate rocks .
- 4. High temperature and ultra-high temperature metamorphism, low, medium and high pressure granulites, anatexis, contact metamorphism.
- Literature
- HALL, Anthony. Igneous petrology. 2nd ed. Essex: Longman Group, 1996, xiv, 551. ISBN 0582230802. info
- MCLANE, Michael. Sedimentology. New York: Oxford University Press, 1995, xiii, 423. ISBN 0195078683. info
- BLATT, Harvey. Sedimentary petrology. 2nd ed. New York: W.H. Freeman, 1992, 514 s. ISBN 0-7167-2273-9. info
- KUKAL, Zdeněk. Základy sedimentologie. 1. vyd. Praha: Academia, 1986, 466 s. info
- KUKAL, Zdeněk. Geology of recent sediments. Praha: Academia, 1970, 490 s. info
- KONOPÁSEK, Jiří. Metamorfní petrologie. 1. vyd. Praha: Karolinum, 1998, 241 s. ISBN 8071846686. info
- Teaching methods
- lecture
- Assessment methods
- Lectures, written tests
- Language of instruction
- Czech
- Further comments (probably available only in Czech)
- The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2010/2011.
The course is taught: every week.
G4021 Petrology II
Faculty of ScienceAutumn 2007 - for the purpose of the accreditation
- Extent and Intensity
- 3/1. 6 credit(s). Type of Completion: zk (examination).
- Teacher(s)
- doc. RNDr. Miroslava Gregerová, CSc. (lecturer)
doc. RNDr. Jana Kotková, CSc. (lecturer)
doc. RNDr. Jindřich Štelcl, CSc. (lecturer)
Mgr. David Buriánek, Ph.D. (lecturer) - Guaranteed by
- doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: Běla Hrbková - Prerequisites
- ( G3021 Petrology I || G3021k Petrology I )&&NOW( G0101 Occupational healt and safety )
The course can be attended only after passing Petrology I. The knowledge of the subject matter is necessary for successful managing of related subjects of magister study. - Course Enrolment Limitations
- The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 60 student(s).
Current registration and enrolment status: enrolled: 0/60, only registered: 0/60, only registered with preference (fields directly associated with the programme): 0/60 - fields of study / plans the course is directly associated with
- there are 37 fields of study the course is directly associated with, display
- Course objectives
- This course is an extension of basic course - Petrology I. Subject deals with problems of genesis of the most important groups of rocks.
- Syllabus
- Igneous rocks:
- Petrotectonic assemblages. Types of crust, continental and oceanic crust, origin of magmas, conditions of ascent and position of magmas, creation of rocks. Chemical restrictions, sources of primary magmas, ascent velocity in lithosphere. Experimental data -petrogenetic meaning of minerals, latice parameters and mineral colours as the source of information of the conditions of mineral creation in rocks, distribution of elements between coexisted minerals, gaseous-liquid inclusions, double-feldspar geothermometer, distribution of Mg, Fe and Ca, Al among the rock forming minerals. Trace elements of igneous rocks and their petrogenetic meaning. Contents of isotopes and the their interpretation.
- Basalts and ultramafic rocks. Types of basalts and their derivatives, basalt occurence: rift volcanism, volcanism of subduction zones, intra-plate volcanicm. Mineral composition, structures and chemical composition of basalts. Ultramafic igneous rocks. Rhyolites and andesites. Types and derivatives of rhyolites and andesites, occurence of rhyolites: hot spots, rifts, transform and tripple faults, volcanic arcs. Occurence of andesites and corresponding rocks. Mineral and chemical composition, structures of andesites. Ultramafic and mafic complexes and corresponding rocks. Shapes of ultramific and ultramafic-mafic rock bodies. Mineral and chemical composition, structures of ultramafic and mafic complexes. Stratified ultramafic complexes, ophiolite complexes, appinite type of ultramafic rocks.
- Granitoidal rock. Composition of granitoidal rocks. Structural and chemical variability. Petrogenesis of granitoidal rocks. Occurence of granitoidal rocks, their tectonic meaning and typology. Formation of granitoidal rocks (fractional crystallization, hybridization, granitization).
- Sedimentary rocks:
- Rock-forming minerals of sedimentary rocks - origin and petrogenesis: clay minerals, silicon oxides and hydroxides, feldspars, carbonates, phosphates, oxides, Fe, Mn, Al-hydroxides, sulfates, chlorides, iron sulfides. Organic matters. Rock-forming organism.
- Origin and evolution of sedimentary structures: Textural characteristic (distribution of grain size, the shapes of sedimentary particles, surface texture of sedimentary particles, matrix, cements and cementation, ooids and pisoids, spherulitic texture, primary and secondary porosity, permeability). Textural classification. Structural classification of sedimentary rocks. Outer and inner structures.
- Origin of sedimentary rocks: weathering processes (mechanical and chemical degradation of rocks, sedimentary cycle, soil formation, erosion. Transport (medium motion, grain flows, water transport, eolian transport, glacial and gravitational processes, orientation of grains). Sedimentation, types of deposition environments. Influence of the tectonic and climatic conditions, sedimentation velocity. Maturity of sediments. Diagenesis of sediments, diagenetic evolution (syndiagenesis, anadiagenesis, epidiagenesis), main phases arising during lithogenesis, geophysical and geochemical conditions of diagenesis, Diagenetic metasomatism. Anchimetamorphism.
- Recent sediments.
- Metamorphic rocks
- Individual types of metamorphic rocks will be treated with emphasis on the geotectonic setting of their genesis. Methods of metamorphic rocks studies aiming at determination of P-T conditions of their formation will be presented. This will include analyses of relationships between metamorphism and deformation, formation and use of mineral zoning, geothermobarometry, geochronology, petrogenetic grids and metamorphic P-T paths. Examples from the Bohemian Massif will be presented.
- 1. Metapelites, quartzofeldspathic rocks (orthogneisses)
- 2. Metabasic and mafic rocks.
- 3. Metacarbonates, calc-silicate rocks .
- 4. High temperature and ultra-high temperature metamorphism, low, medium and high pressure granulites, anatexis, contact metamorphism.
- Literature
- HALL, Anthony. Igneous petrology. 2nd ed. Essex: Longman Group, 1996, xiv, 551. ISBN 0582230802. info
- MCLANE, Michael. Sedimentology. New York: Oxford University Press, 1995, xiii, 423. ISBN 0195078683. info
- BLATT, Harvey. Sedimentary petrology. 2nd ed. New York: W.H. Freeman, 1992, 514 s. ISBN 0-7167-2273-9. info
- KUKAL, Zdeněk. Základy sedimentologie. 1. vyd. Praha: Academia, 1986, 466 s. info
- KUKAL, Zdeněk. Geology of recent sediments. Praha: Academia, 1970, 490 s. info
- KONOPÁSEK, Jiří. Metamorfní petrologie. 1. vyd. Praha: Karolinum, 1998, 241 s. ISBN 8071846686. info
- Assessment methods (in Czech)
- Přednášky a praktická cvičení, každá skupina hornin (magmatické, metamorfované, sedimentární) bude ukončena testem. Ústní zkoušku mohou studenti vykonat pouze po úspěšném zvládnutí písemných části.
- Language of instruction
- Czech
- Further Comments
- The course is taught annually.
The course is taught: every week.
- Enrolment Statistics (recent)