G5021 Regional geology of the CR

Faculty of Science
Spring 2009
Extent and Intensity
3/1. 6 credit(s). Type of Completion: zk (examination).
Teacher(s)
prof. RNDr. Antonín Přichystal, DSc. (lecturer)
prof. RNDr. Lukáš Krmíček, Ph.D. (seminar tutor)
Mgr. Vojtěch Šešulka, 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.
Timetable
Mon 16:00–18:50 G1,01004, Tue 13:00–13:50 Gp,02006, Wed 12:00–12:50 Gp,02006
Prerequisites (in Czech)
! G5020 Regional geology of CR && ! G5021k Regional geology of CR
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 100 student(s).
Current registration and enrolment status: enrolled: 0/100, only registered: 0/100, only registered with preference (fields directly associated with the programme): 0/100
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
The main objectives of the course are following:
a)characterization of the basic geological units in the territory of the Czech Republic;
b)influence of individual orogenetic movements on the development of the Bohemian Massif;
c)age, lithology, magmatic and metamorphic development of Proterozoic and Paleozoic units in the Bohemian Massif;
d)development of the Bohemian Massif in the Upper Carboniferous and Permian;
e)platform development of the Bohemian Massif from the Triassic to the Quaternary;
f)age, lithology and magmatic development of individual units of the West Carpathians in the territory of the Czech Republic;
g)know-how of geological maps, especially with the scale 1:500 000;
h)typical rock types.
Syllabus
  • 1. Principal geological units in the territory of the Czech republic,their delimitation;
  • 2. The Bohemian Massif, general characterization and its subdivision in 6 basic regional geologic regions;
  • 3. The Moldanubian Region;
  • 4. The Kutná Hora - Svratka Region;
  • 5. The Central Bohemian Region;
  • 6. The Lusatian Region;
  • 7. The Saxothuringian region;
  • 8. The Moravo-Silesian Region;
  • 9. Limnic Late Carboniferous and Permian;
  • 10. Platform development of the Bohemian Massif;
  • 10. The Flysh Belt of the West Carpathians;
  • 11. The Vienna Basin;
  • 12. The Carpathian Foredeep.
Literature
  • Chlupáč, I. - Vrána, S. eds. 1994: Regional geological subdivision of the Bohemian Massif on the territory of the Czech Republic. - J.Czech Geol. Soc. 39/1, 127-144. Praha.
  • PŘICHYSTAL, A. Geological structure of the eastern part of the Bohemian Massif. Phanerozoic sedimentary cover. In Kováč, M. & Plašienka, D. (eds.), Geological structure of the Alpine - Carpathian - Pannonian junction and neighbouring slopes of the Bohemian Massif. Bratislava: Comenius University, 2002, p. 7-11. ISBN 80-223-1700-4. info
Assessment methods
Teaching methods: lectures, practical map interpretation It is necessary to pass seminars (searching in geological maps, study of rock samples) that are finished by two written tests. Final oral examen checks also knowledge of geological map and rock samples. It is recommended to pass field excursion focussed on the geology of the Bohemian Massif.
Language of instruction
Czech
Further Comments
Study Materials
The course is taught annually.
Listed among pre-requisites of other courses
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Spring 2011 - only for the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Spring 2010, Spring 2011, Spring 2012, spring 2012 - acreditation, Spring 2013, Spring 2014, Spring 2015, Spring 2016, Spring 2017, spring 2018, Spring 2019, Spring 2020, Spring 2021, Spring 2022, Spring 2023, Spring 2024, Spring 2025.
  • Enrolment Statistics (Spring 2009, recent)
  • Permalink: https://is.muni.cz/course/sci/spring2009/G5021