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Formation
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prof. Ing. Shah Wali Faryad CSc.
Academic staff at Faculty of Science
8 classes
84 publications
Classes
class
Microscopy of Rocks
+1
MG440C12 |
Faculty of Science
class
Microscopy of Minerals and Rocks for Teachers
MG440C11 |
Faculty of Science
class
Fundamentals of Petrology
MG440P04 |
Faculty of Science
class
Petrology of Metamorphic Rocks
+1
MG440P10 |
Faculty of Science
class
Advanced Metamorphic Petrology
MG440P35 |
Faculty of Science
class
Materials Forming the Earth's Crust
MG440P74 |
Faculty of Science
Publications
publication
Ultrahigh-pressure and high-pressure metamorphic terranes in orogenic belts: Reactions, fluids and geological processes: Preface
2013 |
Faculty of Science
publication
The generation of voluminous S-type granites in the Moldanubian unit, Bohemian Massif, by rapid isothermal exhumation of the metapelitic middle crust
2011 |
Faculty of Science
publication
Magmatic and metamorphic evolution of the Shotur Kuh metamorphic complex
2011 |
Faculty of Science
publication
High-pressure partial melting and melt loss in felsic granulites in the Kutna Hora complex, Bohemian Massif (Czech Republic)
2011 |
Faculty of Science
publication
Distribution and geological position of high-/ultrahigh-pressure units within the European Variscan Belt: a review
2011 |
Faculty of Science
publication
Mechanism of formation of atoll garnet during high-pressure metamorphism
2010 |
Faculty of Science
publication
9th International Eclogite Conference
Publication without faculty affiliation
publication
Constraining the P-T path of (U)HP rocks with reaction overstepping during subduction; example from the Western Gneiss Region (Norway)
2022 |
Faculty of Science
publication
Advantages and Limitations of Combined Diffusion-Phase Equilibrium Modelling for Pressure-Temperature-Time History of Metamorphic Rocks
2022 |
Faculty of Science
publication
Dissolution and Reprecipitation of Garnet during Eclogite-facies Metamorphism; Major and Trace Element Transfer during Atoll Garnet Formation
2021 |
Faculty of Science
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