Course Information

G9501 Minerogenetic processes

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

• G8561 Systematic Mineralogy

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

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

• G8561 Systematic Mineralogy

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

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

• G8561 Systematic Mineralogy

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

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

• G8561 Systematic Mineralogy

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

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

• G8561 Systematic Mineralogy

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

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

• G8561 Systematic Mineralogy

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

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

• G8561 Systematic Mineralogy

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

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

• G8561 Systematic Mineralogy

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

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

• G8561 Systematic Mineralogy

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

Extent and Intensity

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

Teacher(s)

doc. RNDr. Zdeněk Losos, CSc. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)

Guaranteed by

doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: Běla Hrbková

Timetable

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

Prerequisites

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

Course Enrolment Limitations

The course is also offered to the students of the fields other than those the course is directly associated with.

fields of study / plans the course is directly associated with

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

Course objectives

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

Syllabus

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

Literature

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

Assessment methods (in Czech)

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

Language of instruction

Czech

Follow-Up Courses

• G8561 Systematic Mineralogy

Further comments (probably available only in Czech)

Study Materials
The course is taught annually.

G9501 Minerogenetic processes

Extent and Intensity

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

Teacher(s)

doc. RNDr. Zdeněk Losos, CSc. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)

Guaranteed by

doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: Běla Hrbková

Timetable

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

• G8561 Systematic Mineralogy

Further comments (probably available only in Czech)

Study Materials
The course is taught annually.

G9501 Minerogenetic processes

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

• G8561 Systematic Mineralogy

Further comments (probably available only in Czech)

The course is taught annually.

G9501 Minerogenetic processes

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

• G8561 Systematic Mineralogy

Further comments (probably available only in Czech)

The course is taught annually.

G9501 Minerogenetic processes

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

• G8561 Systematic Mineralogy

Further comments (probably available only in Czech)

The course is taught annually.

G9501 Minerogenetic processes

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

• G8561 Systematic Mineralogy

Further comments (probably available only in Czech)

The course is taught annually.

G9501 Minerogenetic processes

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

• G8561 Systematic Mineralogy

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

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

• G8561 Systematic Mineralogy

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

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

• G8561 Systematic Mineralogy

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

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

• G8561 Systematic Mineralogy

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

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

• G8561 Systematic Mineralogy

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

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

• G8561 Systematic Mineralogy

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

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

• G8561 Systematic Mineralogy

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

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

• G8561 Systematic Mineralogy

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

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

• G8561 Systematic Mineralogy

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

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

• G8561 Systematic Mineralogy

Further comments (probably available only in Czech)

The course is taught annually.

G9501 Minerogenetic processes

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

• G8561 Systematic Mineralogy

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)