Pyrometamorphism
(Sprache: Englisch)
This extensively revised and updated second edition includes the latest developments in the study of pyrometamorphism. The material covered has been derived from more than 60 new references, which are accompanied by more than 20 new illustrations.
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This extensively revised and updated second edition includes the latest developments in the study of pyrometamorphism. The material covered has been derived from more than 60 new references, which are accompanied by more than 20 new illustrations.
Klappentext zu „Pyrometamorphism “
Pyrometamorphism is a type of contact metamorphism (sanidinite facies) involving very high temperatures that may cause fusion in suitable lithologies at very low pressures. The high temperatures are attained by flow of mafic magma through conduits, by way of spontaneous combustion of coal, carbonaceous sediments, oil and gas, and through the action of lightning strikes. Temperature gradients are typically extreme, varying by several hundred degrees over a few metres or even centimetres. Relatively short periods of heating and cooling create an environment dominated by metastable melting and rapid mineral reaction rates driven by significant temperature overstepping of equilibrium conditions. This results in the formation of a large variety of minerals, many of which are metastable and are only found in pyrometamorphic rocks. The book is aimed for the specialist but also for students and researchers looking for an introduction into pyrometamorphism.
Inhaltsverzeichnis zu „Pyrometamorphism “
Thermal Regimes and Effects.- Quartzofeldspathic Rocks.- Calc-Silicates and Evaporates.- Mafic Rocks.- Anthropogenic and Biomass Pyrometamorphism.- Metastable Mineral Reactions.
Bibliographische Angaben
- Autor: Rodney Grapes
- 2010, 2nd ed., XI, 365 Seiten, Maße: 16 x 24,1 cm, Gebunden, Englisch
- Verlag: Springer, Berlin
- ISBN-10: 3642155871
- ISBN-13: 9783642155871
- Erscheinungsdatum: 02.11.2010
Sprache:
Englisch
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