Pyrometamorphism [Paperback]

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.

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.

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.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 typil3&