G9501 Minerogenetic processes

Faculty of Science
Autumn 2023
Extent and Intensity
2/1/0. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. Mgr. Jan Cempírek, Ph.D. (lecturer)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
Guaranteed by
doc. Mgr. Jan Cempírek, Ph.D.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: Ing. Jana Pechmannová
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Timetable
Fri 24. 11. 14:00–16:00 Gs,-1011, Fri 15. 12. 10:00–16:00 Gs,-1011, Fri 5. 1. 10:00–11:00 G2,02003
Prerequisites
! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && !NOW( G9501k Minerogenetic processes ) && ( (!(PROGRAM(B-GE)||PROGRAM(D-GE4)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemical substances )))
Finishing the Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
fields of study / plans the course is directly associated with
there are 32 fields of study the course is directly associated with, display
Course objectives
At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
Learning outcomes
After the course, student will be able to:
- describe main types of minerogenetic processes;
- describe and assign main mineralization types related to specific minerogenetic processes
- identify main minerogenetic processes that take place during formation of mineral assemblages or mineral deposits;
- apply the gained knowledge to solution of a practical problem during his/her work on diploma thesis
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
    recommended literature
  • OKRUSCH, Martin and Hartwig E. FRIMMEL. Mineralogy : an introduction to minerals, rocks, and mineral deposits. Berlin: Springer, 2020, xi, 719. ISBN 9783662573143. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
    not specified
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • POHL, Walter. Economic geology : principles and practice : metals, minerals, coal and hydrocarbons - introduction to formation and sustainable exploitation of mineral deposits. Chichester: Wiley-Blackwell, 2011, xii, 663. ISBN 9781444336634. URL info
Teaching methods
Lectures and practical exercises.
Assessment methods
Oral examination, practical knowledge of the genesis of mineral samples.
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
Study Materials
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřeno v podzimním semestru 2023/2024.
Teacher's information
http://www.sci.muni.cz/mineralogy
The course is intended primarily for students of the master's degree in geology with a focus on mineralogy.
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021.

G9501 Minerogenetic processes

Faculty of Science
autumn 2021
Extent and Intensity
2/1/0. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. Mgr. Jan Cempírek, Ph.D. (lecturer)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
Mgr. Jan Kocáb (assistant)
Guaranteed by
doc. Mgr. Jan Cempírek, Ph.D.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Timetable
Mon 9:00–10:50 Gs,-1011, Mon 11:00–11:50 Gs,-1011
Prerequisites
! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && !NOW( G9501k Minerogenetic processes ) && ( (!(PROGRAM(B-GE)||PROGRAM(D-GE4)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemical substances )))
Finishing the Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
fields of study / plans the course is directly associated with
there are 32 fields of study the course is directly associated with, display
Course objectives
At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
Learning outcomes
After the course, student will be able to:
- describe main types of minerogenetic processes;
- describe and assign main mineralization types related to specific minerogenetic processes
- identify main minerogenetic processes that take place during formation of mineral assemblages or mineral deposits;
- apply the gained knowledge to solution of a practical problem during his/her work on diploma thesis
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
    recommended literature
  • OKRUSCH, Martin and Hartwig E. FRIMMEL. Mineralogy : an introduction to minerals, rocks, and mineral deposits. Berlin: Springer, 2020, xi, 719. ISBN 9783662573143. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
    not specified
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • POHL, Walter. Economic geology : principles and practice : metals, minerals, coal and hydrocarbons - introduction to formation and sustainable exploitation of mineral deposits. Chichester: Wiley-Blackwell, 2011, xii, 663. ISBN 9781444336634. URL info
Teaching methods
Lectures and practical exercises.
Assessment methods
Oral examination, practical knowledge of the genesis of mineral samples.
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
Study Materials
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřeno v podzimním semestru 2021/2022.
Teacher's information
http://www.sci.muni.cz/mineralogy
The course is intended primarily for students of the master's degree in geology with a focus on mineralogy.
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2019
Extent and Intensity
2/1/0. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. Mgr. Jan Cempírek, Ph.D. (lecturer)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
Mgr. Jan Kocáb (seminar tutor)
Guaranteed by
doc. Mgr. Jan Cempírek, Ph.D.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Timetable
Mon 9:00–10:50 Gs,-1011, Mon 11:00–11:50 Gs,-1011
Prerequisites
! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && !NOW( G9501k Minerogenetic processes ) && ( (!(PROGRAM(B-GE)||PROGRAM(D-GE4)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
Finishing the Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
fields of study / plans the course is directly associated with
there are 32 fields of study the course is directly associated with, display
Course objectives
At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
Learning outcomes
After the course, student will be able to:
- describe main types of minerogenetic processes;
- describe and assign main mineralization types related to specific minerogenetic processes
- identify main minerogenetic processes that take place during formation of mineral assemblages or mineral deposits;
- apply the gained knowledge to solution of a practical problem during his/her work on diploma thesis
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Teaching methods
Lectures and practical exercises.
Assessment methods
Oral examination
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2019/2020.
Teacher's information
http://www.sci.muni.cz/mineralogy
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
autumn 2017
Extent and Intensity
2/1/0. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. Mgr. Jan Cempírek, Ph.D. (lecturer)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
Guaranteed by
doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Timetable
Fri 24. 11. 10:00–16:00 G2,02003
Prerequisites
! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && !NOW( G9501k Minerogenetic processes ) && ( (!(PROGRAM(B-GE)||PROGRAM(D-GE4)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
Termination of Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 16 student(s).
Current registration and enrolment status: enrolled: 0/16, only registered: 0/16, only registered with preference (fields directly associated with the programme): 0/16
fields of study / plans the course is directly associated with
there are 14 fields of study the course is directly associated with, display
Course objectives
At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Teaching methods
Lectures and practical exercises.
Assessment methods
Oral examination
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
Study Materials
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2017/2018.
Teacher's information
http://www.sci.muni.cz/mineralogy
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2015
Extent and Intensity
2/1. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Guaranteed by
doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Timetable
Mon 8:00–9:50 Bp1,01007, Mon 10:00–10:50 Gs,-1011
Prerequisites
! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && !NOW( G9501k Minerogenetic processes ) && ( (!(PROGRAM(B-GE)||PROGRAM(D-GE4)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
Termination of Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 16 student(s).
Current registration and enrolment status: enrolled: 0/16, only registered: 0/16, only registered with preference (fields directly associated with the programme): 0/16
fields of study / plans the course is directly associated with
there are 14 fields of study the course is directly associated with, display
Course objectives
At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Teaching methods
Lectures and practical exercises.
Assessment methods
Oral examination
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
Study Materials
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2015/2016.
Teacher's information
http://www.sci.muni.cz/mineralogy
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2014
Extent and Intensity
2/1. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Mgr. Jakub Výravský, Ph.D. (seminar tutor), prof. RNDr. Milan Novák, CSc. (deputy)
Guaranteed by
doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Prerequisites
! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && !NOW( G9501k Minerogenetic processes ) && ( (!(PROGRAM(B-GE)||PROGRAM(D-GE4)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
Termination of Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 22 student(s).
Current registration and enrolment status: enrolled: 0/22, only registered: 0/22, only registered with preference (fields directly associated with the programme): 0/22
fields of study / plans the course is directly associated with
there are 14 fields of study the course is directly associated with, display
Course objectives
At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
  • NESSE, William D. Introduction to mineralogy. 2nd ed. New York: Oxford University Press, 2012, xv, 480. ISBN 9780199859764. info
  • PHILPOTTS, Anthony R. and Jay J. AGUE. Principles of igneous and metamorphic petrology. 2nd ed. Cambridge: Cambridge University Press, 2009, xviii, 667. ISBN 9780521880060. URL info
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Teaching methods
Lectures and practical exercises.
Assessment methods
Oral examination
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
Study Materials
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2015/2016.
Teacher's information
http://www.sci.muni.cz/mineralogy
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2013
Extent and Intensity
2/1. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Guaranteed by
doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Timetable
Wed 13:00–14:50 Gs,-1011, Wed 15:00–15:50 Gs,-1011
Prerequisites
! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && !NOW( G9501k Minerogenetic processes ) && ( (!(PROGRAM(B-GE)||PROGRAM(D-GE4)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
Termination of Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 22 student(s).
Current registration and enrolment status: enrolled: 0/22, only registered: 0/22, only registered with preference (fields directly associated with the programme): 0/22
fields of study / plans the course is directly associated with
there are 14 fields of study the course is directly associated with, display
Course objectives
At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Teaching methods
Lectures and practical exercises.
Assessment methods
Oral examination
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
Study Materials
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2013/2014.
Teacher's information
http://www.sci.muni.cz/mineralogy
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2011
Extent and Intensity
2/1. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Guaranteed by
doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Timetable
Tue 13:00–14:50 01006, Tue 15:00–15:50 01006
Prerequisites
! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && !NOW( G9501k Minerogenetic processes ) && ( (!(PROGRAM(B-GE)||PROGRAM(D-GE4)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
Termination of Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 11 student(s).
Current registration and enrolment status: enrolled: 0/11, only registered: 0/11, only registered with preference (fields directly associated with the programme): 0/11
fields of study / plans the course is directly associated with
there are 58 fields of study the course is directly associated with, display
Course objectives
At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Teaching methods
Lectures and practical exercises with mineral samples.
Assessment methods
Oral examination
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
Study Materials
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2011/2012.
Teacher's information
http://www.sci.muni.cz/mineralogy
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2009
Extent and Intensity
2/1. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Guaranteed by
doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Timetable
Wed 13:00–14:50 Bp1,01007, Wed 15:00–15:50 Bp1,01007
Prerequisites
! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && !NOW( G9501k Minerogenetic processes ) && ( (!(PROGRAM(B-GE)||PROGRAM(D-GE4)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
Termination of Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 32 student(s).
Current registration and enrolment status: enrolled: 0/32, only registered: 0/32, only registered with preference (fields directly associated with the programme): 0/32
fields of study / plans the course is directly associated with
there are 58 fields of study the course is directly associated with, display
Course objectives
At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Assessment methods
Lectures and practical exercises, oral examination
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
Study Materials
The course is taught once in two years.
Information on the per-term frequency of the course: Výuka proběhne v podzimním semestru akademického roku 2009/2010.
Teacher's information
http://www.sci.muni.cz/mineralogy
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2007
Extent and Intensity
2/1. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Guaranteed by
doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: Běla Hrbková
Timetable
Tue 8:00–9:50 01006, Tue 10:00–10:50 01006
Prerequisites
! G9500 Minerogenetic processes && ( (!(PROGRAM(B-GE)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Manipulation with chemicals )))
Termination of Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
fields of study / plans the course is directly associated with
there are 58 fields of study the course is directly associated with, display
Course objectives
Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Assessment methods (in Czech)
Přednášky, cvičení se vzorky mineralizací. Ústní zkouška z teorie v rozsahu sylabu
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
Study Materials
The course is taught annually.
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2006
Extent and Intensity
2/1. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Guaranteed by
doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: Běla Hrbková
Timetable
Wed 8:00–9:50 01006, Wed 10:00–10:50 01006
Prerequisites
! G9500 Minerogenetic processes
Termination of Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 10 student(s).
Current registration and enrolment status: enrolled: 0/10, only registered: 0/10, only registered with preference (fields directly associated with the programme): 0/10
fields of study / plans the course is directly associated with
there are 58 fields of study the course is directly associated with, display
Course objectives
Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Assessment methods (in Czech)
Přednášky, cvičení se vzorky mineralizací. Ústní zkouška z teorie v rozsahu sylabu
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
Study Materials
The course is taught annually.
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2005
Extent and Intensity
2/1. 3 credit(s) (fasci plus compl plus > 4). Type of Completion: zk (examination).
Teacher(s)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Guaranteed by
doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: Běla Hrbková
Timetable
Wed 8:00–9:50 01006, Wed 10:00–10:50 01006
Prerequisites
! G9500 Minerogenetic processes
Termination of Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 10 student(s).
Current registration and enrolment status: enrolled: 0/10, only registered: 0/10, only registered with preference (fields directly associated with the programme): 0/10
fields of study / plans the course is directly associated with
there are 58 fields of study the course is directly associated with, display
Course objectives
Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Assessment methods (in Czech)
Přednášky, cvičení se vzorky mineralizací. Ústní zkouška z teorie v rozsahu sylabu
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
The course is taught annually.
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2004
Extent and Intensity
2/1. 3 credit(s) (fasci plus compl plus > 4). Type of Completion: zk (examination).
Teacher(s)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Guaranteed by
doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: Běla Hrbková
Timetable
Thu 13:00–15:50 Bp1,01007
Prerequisites
! G9500 Minerogenetic processes
Termination of Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
fields of study / plans the course is directly associated with
Course objectives
Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization.
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization.
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Assessment methods (in Czech)
Přednášky, cvičení ústní zkouška z teorie v rozsahu sylabu
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
The course is taught annually.
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2003
Extent and Intensity
2/1. 3 credit(s) (fasci plus compl plus > 4). Type of Completion: zk (examination).
Teacher(s)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Guaranteed by
doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: Běla Hrbková
Prerequisites
! G9500 Minerogenetic processes
Termination of Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 54 student(s).
Current registration and enrolment status: enrolled: 0/54, only registered: 0/54, only registered with preference (fields directly associated with the programme): 0/54
fields of study / plans the course is directly associated with
Course objectives
Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization.
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization.
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Assessment methods (in Czech)
Přednášky, cvičení ústní zkouška z teorie v rozsahu sylabu
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
The course is taught annually.
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2002
Extent and Intensity
2/1. 3 credit(s) (fasci plus compl plus > 4). Type of Completion: zk (examination).
Teacher(s)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Guaranteed by
doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: Běla Hrbková
Prerequisites
! G9500 Minerogenetic processes
Termination of Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
fields of study / plans the course is directly associated with
Course objectives
Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization.
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization.
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Assessment methods (in Czech)
Přednášky, cvičení ústní zkouška z teorie v rozsahu sylabu
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
The course is taught annually.
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2024

The course is not taught in Autumn 2024

Extent and Intensity
2/1/0. 5 credit(s). Type of Completion: zk (examination).
In-person direct teaching
Teacher(s)
doc. Mgr. Jan Cempírek, Ph.D. (lecturer)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
Guaranteed by
doc. Mgr. Jan Cempírek, Ph.D.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: Ing. Jana Pechmannová
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Prerequisites
! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && !NOW( G9501k Minerogenetic processes ) && ( (!(PROGRAM(B-GE)||PROGRAM(D-GE4)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemical substances )))
Finishing the Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
fields of study / plans the course is directly associated with
there are 32 fields of study the course is directly associated with, display
Course objectives
At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
Learning outcomes
After the course, student will be able to:
- describe main types of minerogenetic processes;
- describe and assign main mineralization types related to specific minerogenetic processes
- identify main minerogenetic processes that take place during formation of mineral assemblages or mineral deposits;
- apply the gained knowledge to solution of a practical problem during his/her work on diploma thesis
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
    recommended literature
  • OKRUSCH, Martin and Hartwig E. FRIMMEL. Mineralogy : an introduction to minerals, rocks, and mineral deposits. Berlin: Springer, 2020, xi, 719. ISBN 9783662573143. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
    not specified
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • POHL, Walter. Economic geology : principles and practice : metals, minerals, coal and hydrocarbons - introduction to formation and sustainable exploitation of mineral deposits. Chichester: Wiley-Blackwell, 2011, xii, 663. ISBN 9781444336634. URL info
Teaching methods
Lectures and practical exercises.
Assessment methods
Oral examination, practical knowledge of the genesis of mineral samples.
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2025/2026.
Teacher's information
http://www.sci.muni.cz/mineralogy
The course is intended primarily for students of the master's degree in geology with a focus on mineralogy.
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2022

The course is not taught in Autumn 2022

Extent and Intensity
2/1/0. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. Mgr. Jan Cempírek, Ph.D. (lecturer)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
Mgr. Jan Kocáb (assistant)
Guaranteed by
doc. Mgr. Jan Cempírek, Ph.D.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Prerequisites
! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && !NOW( G9501k Minerogenetic processes ) && ( (!(PROGRAM(B-GE)||PROGRAM(D-GE4)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemical substances )))
Finishing the Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
fields of study / plans the course is directly associated with
there are 32 fields of study the course is directly associated with, display
Course objectives
At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
Learning outcomes
After the course, student will be able to:
- describe main types of minerogenetic processes;
- describe and assign main mineralization types related to specific minerogenetic processes
- identify main minerogenetic processes that take place during formation of mineral assemblages or mineral deposits;
- apply the gained knowledge to solution of a practical problem during his/her work on diploma thesis
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
    recommended literature
  • OKRUSCH, Martin and Hartwig E. FRIMMEL. Mineralogy : an introduction to minerals, rocks, and mineral deposits. Berlin: Springer, 2020, xi, 719. ISBN 9783662573143. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
    not specified
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • POHL, Walter. Economic geology : principles and practice : metals, minerals, coal and hydrocarbons - introduction to formation and sustainable exploitation of mineral deposits. Chichester: Wiley-Blackwell, 2011, xii, 663. ISBN 9781444336634. URL info
Teaching methods
Lectures and practical exercises.
Assessment methods
Oral examination, practical knowledge of the genesis of mineral samples.
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřeno v podzimním semestru 2021/2022.
Teacher's information
http://www.sci.muni.cz/mineralogy
The course is intended primarily for students of the master's degree in geology with a focus on mineralogy.
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2020

The course is not taught in Autumn 2020

Extent and Intensity
2/1/0. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. Mgr. Jan Cempírek, Ph.D. (lecturer)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
Mgr. Jan Kocáb (assistant)
Guaranteed by
doc. Mgr. Jan Cempírek, Ph.D.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Prerequisites
! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && !NOW( G9501k Minerogenetic processes ) && ( (!(PROGRAM(B-GE)||PROGRAM(D-GE4)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
Finishing the Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
fields of study / plans the course is directly associated with
there are 32 fields of study the course is directly associated with, display
Course objectives
At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
Learning outcomes
After the course, student will be able to:
- describe main types of minerogenetic processes;
- describe and assign main mineralization types related to specific minerogenetic processes
- identify main minerogenetic processes that take place during formation of mineral assemblages or mineral deposits;
- apply the gained knowledge to solution of a practical problem during his/her work on diploma thesis
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Teaching methods
Lectures and practical exercises.
Assessment methods
Oral examination
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřeno v podzimním semestru 2021/2022.
Teacher's information
http://www.sci.muni.cz/mineralogy
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2018

The course is not taught in Autumn 2018

Extent and Intensity
2/1/0. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. Mgr. Jan Cempírek, Ph.D. (lecturer)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
Guaranteed by
doc. Mgr. Jan Cempírek, Ph.D.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Prerequisites
! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && !NOW( G9501k Minerogenetic processes ) && ( (!(PROGRAM(B-GE)||PROGRAM(D-GE4)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
Finishing the Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
fields of study / plans the course is directly associated with
there are 32 fields of study the course is directly associated with, display
Course objectives
At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
Learning outcomes
After the course, student will be able to:
- describe main types of minerogenetic processes;
- describe and assign main mineralization types related to specific minerogenetic processes
- identify main minerogenetic processes that take place during formation of mineral assemblages or mineral deposits;
- apply the gained knowledge to solution of a practical problem during his/her work on diploma thesis
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Teaching methods
Lectures and practical exercises.
Assessment methods
Oral examination
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
Study Materials
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2017/2018.
Teacher's information
http://www.sci.muni.cz/mineralogy
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2016

The course is not taught in Autumn 2016

Extent and Intensity
2/1. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Guaranteed by
doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Prerequisites
! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && !NOW( G9501k Minerogenetic processes ) && ( (!(PROGRAM(B-GE)||PROGRAM(D-GE4)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
Termination of Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 16 student(s).
Current registration and enrolment status: enrolled: 0/16, only registered: 0/16, only registered with preference (fields directly associated with the programme): 0/16
fields of study / plans the course is directly associated with
there are 14 fields of study the course is directly associated with, display
Course objectives
At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Teaching methods
Lectures and practical exercises.
Assessment methods
Oral examination
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2017/2018.
Teacher's information
http://www.sci.muni.cz/mineralogy
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2012

The course is not taught in Autumn 2012

Extent and Intensity
2/1. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Guaranteed by
doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Supplier department: Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Prerequisites
! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && !NOW( G9501k Minerogenetic processes ) && ( (!(PROGRAM(B-GE)||PROGRAM(D-GE4)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
Termination of Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 100 student(s).
Current registration and enrolment status: enrolled: 0/100, only registered: 0/100, only registered with preference (fields directly associated with the programme): 0/100
fields of study / plans the course is directly associated with
there are 14 fields of study the course is directly associated with, display
Course objectives
At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Teaching methods
Lectures and practical exercises.
Assessment methods
Oral examination
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2013/2014.
Teacher's information
http://www.sci.muni.cz/mineralogy
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2010

The course is not taught in Autumn 2010

Extent and Intensity
2/1. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Guaranteed by
doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Prerequisites
! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && !NOW( G9501k Minerogenetic processes ) && ( (!(PROGRAM(B-GE)||PROGRAM(D-GE4)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
Termination of Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
fields of study / plans the course is directly associated with
there are 58 fields of study the course is directly associated with, display
Course objectives
At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Assessment methods
Lectures and practical exercises, oral examination
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2011/2012.
Teacher's information
http://www.sci.muni.cz/mineralogy
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2008

The course is not taught in Autumn 2008

Extent and Intensity
2/1. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Guaranteed by
doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Prerequisites
! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && !NOW( G9501k Minerogenetic processes ) && ( (!(PROGRAM(B-GE)||PROGRAM(D-GE4)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
Termination of Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
fields of study / plans the course is directly associated with
there are 58 fields of study the course is directly associated with, display
Course objectives
At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Assessment methods
Lectures and practical exercises, oral examination
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
The course is taught once in two years.
Information on the per-term frequency of the course: Výuka proběhne v podzimním semestru akademického roku 2009/2010.
Teacher's information
http://www.sci.muni.cz/mineralogy
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2011 - acreditation

The information about the term Autumn 2011 - acreditation is not made public

Extent and Intensity
2/1. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Guaranteed by
doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Prerequisites
! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && !NOW( G9501k Minerogenetic processes ) && ( (!(PROGRAM(B-GE)||PROGRAM(D-GE4)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
Termination of Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
fields of study / plans the course is directly associated with
there are 27 fields of study the course is directly associated with, display
Course objectives
At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals.
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Teaching methods
Lectures and practical exercises.
Assessment methods
Oral examination
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2011/2012.
Teacher's information
http://www.sci.muni.cz/mineralogy
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2007 - for the purpose of the accreditation
Extent and Intensity
2/1. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Guaranteed by
doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: Běla Hrbková
Prerequisites
! G9500 Minerogenetic processes
Termination of Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
The capacity limit for the course is 10 student(s).
Current registration and enrolment status: enrolled: 0/10, only registered: 0/10, only registered with preference (fields directly associated with the programme): 0/10
fields of study / plans the course is directly associated with
there are 58 fields of study the course is directly associated with, display
Course objectives
Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Assessment methods (in Czech)
Přednášky, cvičení se vzorky mineralizací. Ústní zkouška z teorie v rozsahu sylabu
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
The course is taught annually.
The course is also listed under the following terms Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.

G9501 Minerogenetic processes

Faculty of Science
Autumn 2010 - only for the accreditation

The course is not taught in Autumn 2010 - only for the accreditation

Extent and Intensity
2/1. 5 credit(s). Type of Completion: zk (examination).
Teacher(s)
doc. RNDr. Zdeněk Losos, CSc. (lecturer)
prof. RNDr. Milan Novák, CSc. (lecturer)
Guaranteed by
doc. RNDr. Rostislav Melichar, Dr.
Department of Geological Sciences – Earth Sciences Section – Faculty of Science
Contact Person: doc. Mgr. Martin Ivanov, Dr.
Prerequisites
! G9500 Minerogenetic processes && ! G9501k Minerogenetic processes && !NOW( G9501k Minerogenetic processes ) && ( (!(PROGRAM(B-GE)||PROGRAM(D-GE4)||PROGRAM(N-GE)||PROGRAM(D-GE)||PROGRAM(C-CV))) || (NOW( G0101 Occupational healt and safety )&&NOW( C7777 Handling chemicals )))
Termination of Mineralogy I and Mineralogy II courses
Course Enrolment Limitations
The course is also offered to the students of the fields other than those the course is directly associated with.
fields of study / plans the course is directly associated with
there are 58 fields of study the course is directly associated with, display
Course objectives
At the end of this course, students should be able to: use data about Minerogenetic processes to discussion about origin of minerals
Syllabus
  • Origin of granitic pegmatites and their minerals - role of fluida in their orign. The four classes of granitic pegmatites (abyssal, muscovite, rare-element, miarolitic), their origin. Classification of pegmatites of the rare-element class and pegmatite types: rare-earth with allanite-monazite and gadolinite subtypes* beryl with beryl-columbite, beryl-columbite-phosphate subtypes, complex with spodumene, petalite, lepidolite, elbaite, amblygonite subtypes* albite-spodumene, albite. Characteristic of the rare-element pegmatites. Their shape, attitude and size, internal structure, mineralogy, geochemistry, models of internal pegmatite consolidation, origin of metasomatic assemblages, fractionation of elements. Relation of pegmatites to parental granites a their space distribution - regional zonality, pegmatite fields, belts and provinces. Theory of hydrothermal process in confrontation with recent hydrothermal activity (volcanoes, hydrotherms on the oceanic floor): a) T - P bounds of hydrothermal process b) chemistry of hydrothermal medium c) forms of material transportation in hydrothermal medium d) gas-fluid inclusions as indicators of hydrothermal medium Hydrothermal paragenesis - overview of mineralization types (Pb-Zn, Cu ores-in copper bearing sandstones) High temperature mineral paragenesis (formerly designated as pneumatolytic) Magmatogenic paragenesis (intramagmatic - platinoids, Cu-Ni-Fe, Fe-Ti, Ni-Co) Origin of minerals from volcanic exhalations. Disintegration processes (including sulphide deposits). Chemogenic sedimentation (evaporites, Fe-ores). Biomineralization. Origin of minerals during diaganesis. Contact metamorphism - mineral associations. Regional metamorphism - mineral associations. Metasomatic alteration and mineralization. Antropogeneous "mineralizations".
Literature
  • Nesse, William D. Introduction to Mineralogy, 2000, Oxford university press, ISBN 0-19-510691-1, 442 pp.
  • Philpotts, Anthony R. Principles of igneous and metamorphic petrology, 1990, Prentice Hall, ISBN 0-13-691361-X, 498pp., London, Sydney, Toronto.
  • SLAVÍK, František, Jiří NOVÁK and Jaroslav KOKTA. Mineralogie. 5. přeprac. a dopl. vyd. Praha: Academia, 1974, 486 s. info
  • ZOLTAI, Tibor and James H. STOUT. Mineralogy :concepts and principles. Minneapolis, Minnesota: Burgess publishing company, 1985, x, 505 s. ISBN 0-8087-2606-4. info
  • KLEIN, Cornelis and Cornelius S. HURLBUT. Manual of mineralogy : (after James D. Dana). 21st ed. New York: John Wiley & Sons, 1993, xii, 681 s. ISBN 0-471-57452-X. info
Assessment methods
Lectures and practical exercises, oral examination
Language of instruction
Czech
Follow-Up Courses
Further comments (probably available only in Czech)
The course is taught once in two years.
Information on the per-term frequency of the course: Bude otevřen v podzimním semestru 2011/2012.
Teacher's information
http://www.sci.muni.cz/mineralogy
The course is also listed under the following terms Autumn 2007 - for the purpose of the accreditation, Autumn 2002, Autumn 2003, Autumn 2004, Autumn 2005, Autumn 2006, Autumn 2007, Autumn 2009, Autumn 2011, Autumn 2011 - acreditation, Autumn 2013, Autumn 2014, Autumn 2015, autumn 2017, Autumn 2019, autumn 2021, Autumn 2023.
  • Enrolment Statistics (recent)