Petrogenesis of Metamorphic Rocks

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Springer Science & Business Media, 2002 - 341 pages
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Metamorphic rocks make up the largest volume of the Earth. They systematically change their mineralogical composition as a result of tecto-thermal events. The outstanding feature of the 7th edition of this book is the large number of phase diagrams showing the stability relations among minerals and groups of minerals found in metamorphic rocks. The diagrams help to determine the pressure and temperature conditions under which a given collected set of metamorphic rocks may have formed. More than half of the chapters have been completely rewritten or revised. All figures have been edited and improved and recent advances in the field such as multiequilibria thermobarometry and pseudosections were incorporated in the text. The bibliography has been revised and extended, new research publications have also been included. Graduate students will find in depth information on the origin, significance and genesis of metamorphic rocks.
 

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Table des matières

1
17
7
20
4
29
3
47
2
55
Principles of Metamorphic Reactions
62
5
68
Reactions Involving Minerals and Dissolved Components
85
9
203
8
211
LowPressure Metamorphism of Pelites
235
6
242
58
250
67
256
Metamorphism of Marls
259
68
275

1
94
General Considerations
105
4
115
6
121
Retrograde Effects
135
8
154
8
155
5
171
4
179
8
185
6
279
2
288
74
296
5
304
7
311
85
324
Metamorphism of Granitoid Rocks
329
89
337
Droits d'auteur

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Expressions et termes fréquents

Fréquemment cités

Page 338 - WB, 1985. Geochemistry, geochronology and petrology of Monte Mucrone: an example of Eo-Alpine eclogitization of Permian granitoids in the Sesia-Lanzo zone, western Alps, Italy.

Informations bibliographiques