PřF:G9501 Minerogenetic processes - Course Information

G9501 Minerogenetic processes

Extent and Intensity

2/1. 5 credit(s). Type of Completion: zk (examination).

Teacher(s)

doc. RNDr. Zdeněk Losos, CSc. (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: Běla Hrbková

Timetable

Tue 8:00–9:50 01006, Tue 10:00–10:50 01006

Prerequisites

! G9500 Minerogenetic processes && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Manipulation with chemicals )))
Termination of Mineralogy I and Mineralogy II courses

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 58 fields of study the course is directly associated with, display

Course objectives

Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".

Syllabus

• Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".

Literature

• Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
• Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
• SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
• ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
• KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info

Assessment methods (in Czech)

Přednášky, cvičení se vzorky mineralizací. Ústní zkouška z teorie v rozsahu sylabu

Language of instruction

Czech

Follow-Up Courses

• G8561 Systematic Mineralogy

Further comments (probably available only in Czech)

Study Materials
The course is taught annually.

• Enrolment Statistics (Autumn 2007, recent)
  
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