1000 DegreesC) 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.
General
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