G9501 Minerogenetic processes
Faculty of ScienceAutumn 2023
- Extent and Intensity
- 2/1/0. 5 credit(s). Type of Completion: zk (examination).
- Teacher(s)
- doc. Mgr. Jan Cempírek, Ph.D. (lecturer)
doc. RNDr. Zdeněk Losos, CSc. (lecturer) - Guaranteed by
- doc. Mgr. Jan Cempírek, Ph.D.
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
- Fri 24. 11. 14:00–16:00 Gs,-1011, Fri 15. 12. 10:00–16:00 Gs,-1011, Fri 5. 1. 10:00–11:00 G2,02003
- Prerequisites
- ! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && ! NOW ( G9501k Minerogenetic processes ) && ( (!( PROGRAM ( B - GE )|| PROGRAM ( D - GE4 )|| PROGRAM ( N - GE )|| PROGRAM ( D - GE )|| PROGRAM ( C - CV ))) || ( NOW ( G0101 Occupational healt and safety )&& NOW ( C7777 Handling chemical substances )))
Finishing the 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 32 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
- Learning outcomes
- After the course, student will be able to:
- describe main types of minerogenetic processes;
- describe and assign main mineralization types related to specific minerogenetic processes
- identify main minerogenetic processes that take place during formation of mineral assemblages or mineral deposits;
- apply the gained knowledge to solution of a practical problem during his/her work on diploma thesis - 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
- recommended literature
- OKRUSCH, Martin and Hartwig E. FRIMMEL. Mineralogy : an introduction to minerals, rocks, and mineral deposits. Berlin: Springer, 2020, xi, 719. ISBN 9783662573143. 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
- not specified
- Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
- 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
- SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
- Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
- POHL, Walter. Economic geology : principles and practice : metals, minerals, coal and hydrocarbons - introduction to formation and sustainable exploitation of mineral deposits. Chichester: Wiley-Blackwell, 2011, xii, 663. ISBN 9781444336634. URL info
- Teaching methods
- Lectures and practical exercises.
- Assessment methods
- Oral examination, practical knowledge of the genesis of mineral samples.
- Language of instruction
- Czech
- Follow-Up Courses
- 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 otevřeno v podzimním semestru 2023/2024. - Teacher's information
- http://www.sci.muni.cz/mineralogy
The course is intended primarily for students of the master's degree in geology with a focus on mineralogy.
G9501 Minerogenetic processes
Faculty of Scienceautumn 2021
- Extent and Intensity
- 2/1/0. 5 credit(s). Type of Completion: zk (examination).
- Teacher(s)
- doc. Mgr. Jan Cempírek, Ph.D. (lecturer)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
Mgr. Jan Kocáb (assistant) - Guaranteed by
- doc. Mgr. Jan Cempírek, Ph.D.
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 9:00–10:50 Gs,-1011, Mon 11:00–11:50 Gs,-1011
- Prerequisites
- ! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && ! NOW ( G9501k Minerogenetic processes ) && ( (!( PROGRAM ( B - GE )|| PROGRAM ( D - GE4 )|| PROGRAM ( N - GE )|| PROGRAM ( D - GE )|| PROGRAM ( C - CV ))) || ( NOW ( G0101 Occupational healt and safety )&& NOW ( C7777 Handling chemical substances )))
Finishing the 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 32 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
- Learning outcomes
- After the course, student will be able to:
- describe main types of minerogenetic processes;
- describe and assign main mineralization types related to specific minerogenetic processes
- identify main minerogenetic processes that take place during formation of mineral assemblages or mineral deposits;
- apply the gained knowledge to solution of a practical problem during his/her work on diploma thesis - 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
- recommended literature
- OKRUSCH, Martin and Hartwig E. FRIMMEL. Mineralogy : an introduction to minerals, rocks, and mineral deposits. Berlin: Springer, 2020, xi, 719. ISBN 9783662573143. 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
- not specified
- Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
- 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
- SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
- Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
- POHL, Walter. Economic geology : principles and practice : metals, minerals, coal and hydrocarbons - introduction to formation and sustainable exploitation of mineral deposits. Chichester: Wiley-Blackwell, 2011, xii, 663. ISBN 9781444336634. URL info
- Teaching methods
- Lectures and practical exercises.
- Assessment methods
- Oral examination, practical knowledge of the genesis of mineral samples.
- Language of instruction
- Czech
- Follow-Up Courses
- 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 otevřeno v podzimním semestru 2021/2022. - Teacher's information
- http://www.sci.muni.cz/mineralogy
The course is intended primarily for students of the master's degree in geology with a focus on mineralogy.
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2019
- Extent and Intensity
- 2/1/0. 5 credit(s). Type of Completion: zk (examination).
- Teacher(s)
- doc. Mgr. Jan Cempírek, Ph.D. (lecturer)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
Mgr. Jan Kocáb (seminar tutor) - Guaranteed by
- doc. Mgr. Jan Cempírek, Ph.D.
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 9:00–10:50 Gs,-1011, Mon 11:00–11:50 Gs,-1011
- Prerequisites
- ! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && ! NOW ( G9501k Minerogenetic processes ) && ( (!( PROGRAM ( B - GE )|| PROGRAM ( D - GE4 )|| PROGRAM ( N - GE )|| PROGRAM ( D - GE )|| PROGRAM ( C - CV ))) || ( NOW ( G0101 Occupational healt and safety )&& NOW ( C7777 Handling chemicals )))
Finishing the 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 32 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
- Learning outcomes
- After the course, student will be able to:
- describe main types of minerogenetic processes;
- describe and assign main mineralization types related to specific minerogenetic processes
- identify main minerogenetic processes that take place during formation of mineral assemblages or mineral deposits;
- apply the gained knowledge to solution of a practical problem during his/her work on diploma thesis - 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
- Teaching methods
- Lectures and practical exercises.
- Assessment methods
- Oral examination
- Language of instruction
- Czech
- Follow-Up Courses
- 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 2019/2020. - Teacher's information
- http://www.sci.muni.cz/mineralogy
G9501 Minerogenetic processes
Faculty of Scienceautumn 2017
- Extent and Intensity
- 2/1/0. 5 credit(s). Type of Completion: zk (examination).
- Teacher(s)
- doc. Mgr. Jan Cempírek, Ph.D. (lecturer)
doc. RNDr. Zdeněk Losos, 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
- Fri 24. 11. 10:00–16:00 G2,02003
- Prerequisites
- ! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && ! NOW ( G9501k Minerogenetic processes ) && ( (!( PROGRAM ( B - GE )|| PROGRAM ( D - GE4 )|| PROGRAM ( N - GE )|| PROGRAM ( D - GE )|| PROGRAM ( C - CV ))) || ( NOW ( G0101 Occupational healt and safety )&& NOW ( C7777 Handling 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.
The capacity limit for the course is 16 student(s).
Current registration and enrolment status: enrolled: 0/16, only registered: 0/16, only registered with preference (fields directly associated with the programme): 0/16 - 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: use data about Minerogenetic processes to discussion about origin of minerals.
- 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
- Teaching methods
- Lectures and practical exercises.
- Assessment methods
- Oral examination
- Language of instruction
- Czech
- Follow-Up Courses
- 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 2017/2018. - Teacher's information
- http://www.sci.muni.cz/mineralogy
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2015
- 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: 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, Mon 10:00–10:50 Gs,-1011
- Prerequisites
- ! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && ! NOW ( G9501k Minerogenetic processes ) && ( (!( PROGRAM ( B - GE )|| PROGRAM ( D - GE4 )|| PROGRAM ( N - GE )|| PROGRAM ( D - GE )|| PROGRAM ( C - CV ))) || ( NOW ( G0101 Occupational healt and safety )&& NOW ( C7777 Handling 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.
The capacity limit for the course is 16 student(s).
Current registration and enrolment status: enrolled: 0/16, only registered: 0/16, only registered with preference (fields directly associated with the programme): 0/16 - 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: use data about Minerogenetic processes to discussion about origin of minerals.
- 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
- Teaching methods
- Lectures and practical exercises.
- Assessment methods
- Oral examination
- Language of instruction
- Czech
- Follow-Up Courses
- 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 2015/2016. - Teacher's information
- http://www.sci.muni.cz/mineralogy
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2014
- 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)
Mgr. Jakub Výravský, Ph.D. (seminar tutor), prof. RNDr. Milan Novák, CSc. (deputy) - 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
- ! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && ! NOW ( G9501k Minerogenetic processes ) && ( (!( PROGRAM ( B - GE )|| PROGRAM ( D - GE4 )|| PROGRAM ( N - GE )|| PROGRAM ( D - GE )|| PROGRAM ( C - CV ))) || ( NOW ( G0101 Occupational healt and safety )&& NOW ( C7777 Handling 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.
The capacity limit for the course is 22 student(s).
Current registration and enrolment status: enrolled: 0/22, only registered: 0/22, only registered with preference (fields directly associated with the programme): 0/22 - 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: use data about Minerogenetic processes to discussion about origin of minerals.
- 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. 2nd ed. New York: Oxford University Press, 2012, xv, 480. ISBN 9780199859764. info
- PHILPOTTS, Anthony R. and Jay J. AGUE. Principles of igneous and metamorphic petrology. 2nd ed. Cambridge: Cambridge University Press, 2009, xviii, 667. ISBN 9780521880060. URL info
- 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
- Teaching methods
- Lectures and practical exercises.
- Assessment methods
- Oral examination
- Language of instruction
- Czech
- Follow-Up Courses
- 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 2015/2016. - Teacher's information
- http://www.sci.muni.cz/mineralogy
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2013
- 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: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science - Timetable
- Wed 13:00–14:50 Gs,-1011, Wed 15:00–15:50 Gs,-1011
- Prerequisites
- ! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && ! NOW ( G9501k Minerogenetic processes ) && ( (!( PROGRAM ( B - GE )|| PROGRAM ( D - GE4 )|| PROGRAM ( N - GE )|| PROGRAM ( D - GE )|| PROGRAM ( C - CV ))) || ( NOW ( G0101 Occupational healt and safety )&& NOW ( C7777 Handling 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.
The capacity limit for the course is 22 student(s).
Current registration and enrolment status: enrolled: 0/22, only registered: 0/22, only registered with preference (fields directly associated with the programme): 0/22 - 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: use data about Minerogenetic processes to discussion about origin of minerals.
- 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
- Teaching methods
- Lectures and practical exercises.
- Assessment methods
- Oral examination
- Language of instruction
- Czech
- Follow-Up Courses
- 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 2013/2014. - Teacher's information
- http://www.sci.muni.cz/mineralogy
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2011
- 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: doc. Mgr. Martin Ivanov, Dr. - Timetable
- Tue 13:00–14:50 01006, Tue 15:00–15:50 01006
- Prerequisites
- ! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && ! NOW ( G9501k Minerogenetic processes ) && ( (!( PROGRAM ( B - GE )|| PROGRAM ( D - GE4 )|| PROGRAM ( N - GE )|| PROGRAM ( D - GE )|| PROGRAM ( C - CV ))) || ( NOW ( G0101 Occupational healt and safety )&& NOW ( C7777 Handling 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.
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 58 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals
- 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
- Teaching methods
- Lectures and practical exercises with mineral samples.
- Assessment methods
- Oral examination
- Language of instruction
- Czech
- Follow-Up Courses
- 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 2011/2012. - Teacher's information
- http://www.sci.muni.cz/mineralogy
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2009
- 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: doc. Mgr. Martin Ivanov, Dr. - Timetable
- Wed 13:00–14:50 Bp1,01007, Wed 15:00–15:50 Bp1,01007
- Prerequisites
- ! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && ! NOW ( G9501k Minerogenetic processes ) && ( (!( PROGRAM ( B - GE )|| PROGRAM ( D - GE4 )|| PROGRAM ( N - GE )|| PROGRAM ( D - GE )|| PROGRAM ( C - CV ))) || ( NOW ( G0101 Occupational healt and safety )&& NOW ( C7777 Handling 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.
The capacity limit for the course is 32 student(s).
Current registration and enrolment status: enrolled: 0/32, only registered: 0/32, only registered with preference (fields directly associated with the programme): 0/32 - 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
- At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals
- 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
- Lectures and practical exercises, oral examination
- Language of instruction
- Czech
- Follow-Up Courses
- 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. - Teacher's information
- http://www.sci.muni.cz/mineralogy
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2007
- 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
- Further comments (probably available only in Czech)
- Study Materials
The course is taught annually.
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2006
- 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
- Wed 8:00–9:50 01006, Wed 10:00–10:50 01006
- Prerequisites
- ! G9500 Minerogenetic processes
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.
The capacity limit for the course is 10 student(s).
Current registration and enrolment status: enrolled: 0/10, only registered: 0/10, only registered with preference (fields directly associated with the programme): 0/10 - 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
- Further comments (probably available only in Czech)
- Study Materials
The course is taught annually.
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2005
- Extent and Intensity
- 2/1. 3 credit(s) (fasci plus compl plus > 4). 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
- Wed 8:00–9:50 01006, Wed 10:00–10:50 01006
- Prerequisites
- ! G9500 Minerogenetic processes
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.
The capacity limit for the course is 10 student(s).
Current registration and enrolment status: enrolled: 0/10, only registered: 0/10, only registered with preference (fields directly associated with the programme): 0/10 - 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
- Further comments (probably available only in Czech)
- The course is taught annually.
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2004
- Extent and Intensity
- 2/1. 3 credit(s) (fasci plus compl plus > 4). 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
- Thu 13:00–15:50 Bp1,01007
- Prerequisites
- ! G9500 Minerogenetic processes
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
- Geology, Hydrogeology and Geochemistry (programme PřF, M-GE)
- Geology, Hydrogeology and Geochemistry (programme PřF, N-GE)
- 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.
- 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.
- 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 ústní zkouška z teorie v rozsahu sylabu
- Language of instruction
- Czech
- Follow-Up Courses
- Further comments (probably available only in Czech)
- The course is taught annually.
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2003
- Extent and Intensity
- 2/1. 3 credit(s) (fasci plus compl plus > 4). 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 - Prerequisites
- ! G9500 Minerogenetic processes
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.
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, M-GE)
- Geology, Hydrogeology and Geochemistry (programme PřF, N-GE)
- 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.
- 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.
- 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 ústní zkouška z teorie v rozsahu sylabu
- Language of instruction
- Czech
- Follow-Up Courses
- Further comments (probably available only in Czech)
- The course is taught annually.
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2002
- Extent and Intensity
- 2/1. 3 credit(s) (fasci plus compl plus > 4). 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 - Prerequisites
- ! G9500 Minerogenetic processes
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
- Geology, Hydrogeology and Geochemistry (programme PřF, M-GE)
- Geology, Hydrogeology and Geochemistry (programme PřF, N-GE)
- 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.
- 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.
- 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 ústní zkouška z teorie v rozsahu sylabu
- Language of instruction
- Czech
- Follow-Up Courses
- Further comments (probably available only in Czech)
- The course is taught annually.
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2024
The course is not taught in Autumn 2024
- Extent and Intensity
- 2/1/0. 5 credit(s). Type of Completion: zk (examination).
- Teacher(s)
- doc. Mgr. Jan Cempírek, Ph.D. (lecturer)
doc. RNDr. Zdeněk Losos, CSc. (lecturer) - Guaranteed by
- doc. Mgr. Jan Cempírek, Ph.D.
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
- ! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && ! NOW ( G9501k Minerogenetic processes ) && ( (!( PROGRAM ( B - GE )|| PROGRAM ( D - GE4 )|| PROGRAM ( N - GE )|| PROGRAM ( D - GE )|| PROGRAM ( C - CV ))) || ( NOW ( G0101 Occupational healt and safety )&& NOW ( C7777 Handling chemical substances )))
Finishing the 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 32 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
- Learning outcomes
- After the course, student will be able to:
- describe main types of minerogenetic processes;
- describe and assign main mineralization types related to specific minerogenetic processes
- identify main minerogenetic processes that take place during formation of mineral assemblages or mineral deposits;
- apply the gained knowledge to solution of a practical problem during his/her work on diploma thesis - 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
- recommended literature
- OKRUSCH, Martin and Hartwig E. FRIMMEL. Mineralogy : an introduction to minerals, rocks, and mineral deposits. Berlin: Springer, 2020, xi, 719. ISBN 9783662573143. 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
- not specified
- Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
- 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
- SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
- Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
- POHL, Walter. Economic geology : principles and practice : metals, minerals, coal and hydrocarbons - introduction to formation and sustainable exploitation of mineral deposits. Chichester: Wiley-Blackwell, 2011, xii, 663. ISBN 9781444336634. URL info
- Teaching methods
- Lectures and practical exercises.
- Assessment methods
- Oral examination, practical knowledge of the genesis of mineral samples.
- Language of instruction
- Czech
- Follow-Up Courses
- 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 2025/2026. - Teacher's information
- http://www.sci.muni.cz/mineralogy
The course is intended primarily for students of the master's degree in geology with a focus on mineralogy.
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2022
The course is not taught in Autumn 2022
- Extent and Intensity
- 2/1/0. 5 credit(s). Type of Completion: zk (examination).
- Teacher(s)
- doc. Mgr. Jan Cempírek, Ph.D. (lecturer)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
Mgr. Jan Kocáb (assistant) - Guaranteed by
- doc. Mgr. Jan Cempírek, Ph.D.
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
- ! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && ! NOW ( G9501k Minerogenetic processes ) && ( (!( PROGRAM ( B - GE )|| PROGRAM ( D - GE4 )|| PROGRAM ( N - GE )|| PROGRAM ( D - GE )|| PROGRAM ( C - CV ))) || ( NOW ( G0101 Occupational healt and safety )&& NOW ( C7777 Handling chemical substances )))
Finishing the 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 32 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
- Learning outcomes
- After the course, student will be able to:
- describe main types of minerogenetic processes;
- describe and assign main mineralization types related to specific minerogenetic processes
- identify main minerogenetic processes that take place during formation of mineral assemblages or mineral deposits;
- apply the gained knowledge to solution of a practical problem during his/her work on diploma thesis - 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
- recommended literature
- OKRUSCH, Martin and Hartwig E. FRIMMEL. Mineralogy : an introduction to minerals, rocks, and mineral deposits. Berlin: Springer, 2020, xi, 719. ISBN 9783662573143. 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
- not specified
- Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
- 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
- SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
- Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
- POHL, Walter. Economic geology : principles and practice : metals, minerals, coal and hydrocarbons - introduction to formation and sustainable exploitation of mineral deposits. Chichester: Wiley-Blackwell, 2011, xii, 663. ISBN 9781444336634. URL info
- Teaching methods
- Lectures and practical exercises.
- Assessment methods
- Oral examination, practical knowledge of the genesis of mineral samples.
- Language of instruction
- Czech
- Follow-Up Courses
- 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 otevřeno v podzimním semestru 2021/2022. - Teacher's information
- http://www.sci.muni.cz/mineralogy
The course is intended primarily for students of the master's degree in geology with a focus on mineralogy.
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2020
The course is not taught in Autumn 2020
- Extent and Intensity
- 2/1/0. 5 credit(s). Type of Completion: zk (examination).
- Teacher(s)
- doc. Mgr. Jan Cempírek, Ph.D. (lecturer)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
Mgr. Jan Kocáb (assistant) - Guaranteed by
- doc. Mgr. Jan Cempírek, Ph.D.
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
- ! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && ! NOW ( G9501k Minerogenetic processes ) && ( (!( PROGRAM ( B - GE )|| PROGRAM ( D - GE4 )|| PROGRAM ( N - GE )|| PROGRAM ( D - GE )|| PROGRAM ( C - CV ))) || ( NOW ( G0101 Occupational healt and safety )&& NOW ( C7777 Handling chemicals )))
Finishing the 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 32 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
- Learning outcomes
- After the course, student will be able to:
- describe main types of minerogenetic processes;
- describe and assign main mineralization types related to specific minerogenetic processes
- identify main minerogenetic processes that take place during formation of mineral assemblages or mineral deposits;
- apply the gained knowledge to solution of a practical problem during his/her work on diploma thesis - 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
- Teaching methods
- Lectures and practical exercises.
- Assessment methods
- Oral examination
- Language of instruction
- Czech
- Follow-Up Courses
- 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 otevřeno v podzimním semestru 2021/2022. - Teacher's information
- http://www.sci.muni.cz/mineralogy
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2018
The course is not taught in Autumn 2018
- Extent and Intensity
- 2/1/0. 5 credit(s). Type of Completion: zk (examination).
- Teacher(s)
- doc. Mgr. Jan Cempírek, Ph.D. (lecturer)
doc. RNDr. Zdeněk Losos, CSc. (lecturer) - Guaranteed by
- doc. Mgr. Jan Cempírek, Ph.D.
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
- ! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && ! NOW ( G9501k Minerogenetic processes ) && ( (!( PROGRAM ( B - GE )|| PROGRAM ( D - GE4 )|| PROGRAM ( N - GE )|| PROGRAM ( D - GE )|| PROGRAM ( C - CV ))) || ( NOW ( G0101 Occupational healt and safety )&& NOW ( C7777 Handling chemicals )))
Finishing the 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 32 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
- Learning outcomes
- After the course, student will be able to:
- describe main types of minerogenetic processes;
- describe and assign main mineralization types related to specific minerogenetic processes
- identify main minerogenetic processes that take place during formation of mineral assemblages or mineral deposits;
- apply the gained knowledge to solution of a practical problem during his/her work on diploma thesis - 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
- Teaching methods
- Lectures and practical exercises.
- Assessment methods
- Oral examination
- Language of instruction
- Czech
- Follow-Up Courses
- 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 2017/2018. - Teacher's information
- http://www.sci.muni.cz/mineralogy
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2016
The course is not taught in Autumn 2016
- 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: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science - Prerequisites
- ! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && ! NOW ( G9501k Minerogenetic processes ) && ( (!( PROGRAM ( B - GE )|| PROGRAM ( D - GE4 )|| PROGRAM ( N - GE )|| PROGRAM ( D - GE )|| PROGRAM ( C - CV ))) || ( NOW ( G0101 Occupational healt and safety )&& NOW ( C7777 Handling 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.
The capacity limit for the course is 16 student(s).
Current registration and enrolment status: enrolled: 0/16, only registered: 0/16, only registered with preference (fields directly associated with the programme): 0/16 - 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: use data about Minerogenetic processes to discussion about origin of minerals.
- 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
- Teaching methods
- Lectures and practical exercises.
- Assessment methods
- Oral examination
- Language of instruction
- Czech
- Follow-Up Courses
- 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 2017/2018. - Teacher's information
- http://www.sci.muni.cz/mineralogy
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2012
The course is not taught in Autumn 2012
- 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: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science - Prerequisites
- ! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && ! NOW ( G9501k Minerogenetic processes ) && ( (!( PROGRAM ( B - GE )|| PROGRAM ( D - GE4 )|| PROGRAM ( N - GE )|| PROGRAM ( D - GE )|| PROGRAM ( C - CV ))) || ( NOW ( G0101 Occupational healt and safety )&& NOW ( C7777 Handling 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.
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 14 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
- 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
- Teaching methods
- Lectures and practical exercises.
- Assessment methods
- Oral examination
- Language of instruction
- Czech
- Follow-Up Courses
- 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 2013/2014. - Teacher's information
- http://www.sci.muni.cz/mineralogy
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2010
The course is not taught in Autumn 2010
- 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: doc. Mgr. Martin Ivanov, Dr. - Prerequisites
- ! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && ! NOW ( G9501k Minerogenetic processes ) && ( (!( PROGRAM ( B - GE )|| PROGRAM ( D - GE4 )|| PROGRAM ( N - GE )|| PROGRAM ( D - GE )|| PROGRAM ( C - CV ))) || ( NOW ( G0101 Occupational healt and safety )&& NOW ( C7777 Handling 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
- At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals
- 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
- Lectures and practical exercises, oral examination
- Language of instruction
- Czech
- Follow-Up Courses
- 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 2011/2012. - Teacher's information
- http://www.sci.muni.cz/mineralogy
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2008
The course is not taught in Autumn 2008
- 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: doc. Mgr. Martin Ivanov, Dr. - Prerequisites
- ! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && ! NOW ( G9501k Minerogenetic processes ) && ( (!( PROGRAM ( B - GE )|| PROGRAM ( D - GE4 )|| PROGRAM ( N - GE )|| PROGRAM ( D - GE )|| PROGRAM ( C - CV ))) || ( NOW ( G0101 Occupational healt and safety )&& NOW ( C7777 Handling 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
- At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals
- 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
- Lectures and practical exercises, oral examination
- Language of instruction
- Czech
- Follow-Up Courses
- 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 2009/2010. - Teacher's information
- http://www.sci.muni.cz/mineralogy
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2011 - acreditation
The information about the term Autumn 2011 - acreditation is not made public
- 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: doc. Mgr. Martin Ivanov, Dr. - Prerequisites
- ! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && ! NOW ( G9501k Minerogenetic processes ) && ( (!( PROGRAM ( B - GE )|| PROGRAM ( D - GE4 )|| PROGRAM ( N - GE )|| PROGRAM ( D - GE )|| PROGRAM ( C - CV ))) || ( NOW ( G0101 Occupational healt and safety )&& NOW ( C7777 Handling 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 27 fields of study the course is directly associated with, display
- Course objectives
- At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
- 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
- Teaching methods
- Lectures and practical exercises.
- Assessment methods
- Oral examination
- Language of instruction
- Czech
- Follow-Up Courses
- 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 2011/2012. - Teacher's information
- http://www.sci.muni.cz/mineralogy
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2007 - for the purpose of the accreditation
- 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 - Prerequisites
- ! G9500 Minerogenetic processes
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.
The capacity limit for the course is 10 student(s).
Current registration and enrolment status: enrolled: 0/10, only registered: 0/10, only registered with preference (fields directly associated with the programme): 0/10 - 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
- Further comments (probably available only in Czech)
- The course is taught annually.
G9501 Minerogenetic processes
Faculty of ScienceAutumn 2010 - only for the accreditation
The course is not taught in Autumn 2010 - only for the accreditation
- 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: doc. Mgr. Martin Ivanov, Dr. - Prerequisites
- ! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && ! NOW ( G9501k Minerogenetic processes ) && ( (!( PROGRAM ( B - GE )|| PROGRAM ( D - GE4 )|| PROGRAM ( N - GE )|| PROGRAM ( D - GE )|| PROGRAM ( C - CV ))) || ( NOW ( G0101 Occupational healt and safety )&& NOW ( C7777 Handling 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
- At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals
- 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
- Lectures and practical exercises, oral examination
- Language of instruction
- Czech
- Follow-Up Courses
- 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 2011/2012. - Teacher's information
- http://www.sci.muni.cz/mineralogy
- Enrolment Statistics (recent)