Pyrometamorphism
Rodney Grapes
Pyrometamorphism occurs at very high temperatures (800 - > 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.
Categorias:
Ano:
2006
Edição:
1
Editora:
Springer
Idioma:
english
Páginas:
280
ISBN 10:
3540294538
ISBN 13:
9783540294535
Arquivo:
PDF, 10.25 MB
IPFS:
,
english, 2006
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