Petrogenesis of Metamorphic RocksMetamorphic 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 |
324 | |
Metamorphism of Granitoid Rocks | 329 |
337 | |
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Expressions et termes fréquents
addition amounts amphibole amphibolite facies biotite blueschist boundary calcite calculated carbonate changes characteristic chemical chlorite components composition contain Contrib Mineral Petrol crust curve defined depends diagram diopside discussed dolomite eclogites effect equilibrium example excess exchange experimental field fluid follows formation forsterite garnet geological given grade granulite facies greenschist facies H₂O heat higher hydrated important increasing invariant involving isograd Italy K-feldspar kbar kyanite limit lower mantle marbles melting meta Metamorph Geol metamorphic rocks metapelites mineral assemblages mineralogy muscovite Note occur orogenic path pelitic phase plagioclase present pressure processes produced prograde projection pure quartz range reaction reference regional relationships replaced represents result schists shown in Fig shows sillimanite solution space stable structure surface Table talc temperature thermodynamic tion tremolite typical ultramafic rocks upper volume zone
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.