Pyrometamorphism [recurso electrónico] / by Rodney Grapes.

Por: Grapes, Rodney [author.]Colaborador(es): SpringerLink (Online service)Tipo de material: Texto

TextoEditor: Berlin, Heidelberg : Springer Berlin Heidelberg : Imprint: Springer, 2010Edición: 2Descripción: XI, 365 p. online resourceTipo de contenido: text Tipo de medio: computer Tipo de portador: online resourceISBN: 9783642155888Tema(s): Geography | Geochemistry | Mines and mineral resources | Mineralogy | Earth Sciences | Mineralogy | Mineral Resources | GeochemistryFormatos físicos adicionales: Printed edition:: Sin títuloClasificación CDD: 549 Clasificación LoC:QE351-399.2Recursos en línea: Libro electrónico Texto

Contenidos:

Thermal Regimes and Effects -- Quartzofeldspathic Rocks -- Calc-Silicates and Evaporates -- Mafic Rocks -- Anthropogenic and Biomass Pyrometamorphism -- Metastable Mineral Reactions.

En: Springer eBooksResumen: 1000 °C) and low pressures (< 2 kb) and typically results in the formation of "burnt" and fused rocks termed buchites, paralavas, clinkers and fulgarites. It is typically associated with shallow basaltic intrusions (contact aureoles, xenoliths,) combustion of carbonaceous matter, lightning strikes, and is also found in meteorites. During pyrometamorphism, the sequence of heating and cooling is greatly condensed favouring the preservation of a variety of stranded reaction microstructures that reflect disequilibrium reaction kinetics with metastable and mineral crystallisation. This second edition includes the latest developments in the study of pyrometamorphism derived from over 60 new references and accompanied with over 20 new illustrations.

Existencias ( 1 )
Notas de título ( 3 )

Existencias
Tipo de ítem	Biblioteca actual	Colección	Signatura	Copia número	Estado	Fecha de vencimiento	Código de barras
Libro Electrónico	Biblioteca Electrónica	Colección de Libros Electrónicos	QE351 -399.2 (Browse shelf(Abre debajo))	1	No para préstamo		375074-2001

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Thermal Regimes and Effects -- Quartzofeldspathic Rocks -- Calc-Silicates and Evaporates -- Mafic Rocks -- Anthropogenic and Biomass Pyrometamorphism -- Metastable Mineral Reactions.

1000 °C) and low pressures (< 2 kb) and typically results in the formation of "burnt" and fused rocks termed buchites, paralavas, clinkers and fulgarites. It is typically associated with shallow basaltic intrusions (contact aureoles, xenoliths,) combustion of carbonaceous matter, lightning strikes, and is also found in meteorites. During pyrometamorphism, the sequence of heating and cooling is greatly condensed favouring the preservation of a variety of stranded reaction microstructures that reflect disequilibrium reaction kinetics with metastable and mineral crystallisation. This second edition includes the latest developments in the study of pyrometamorphism derived from over 60 new references and accompanied with over 20 new illustrations.