Ultrahigh Pressure Metamorphism

الغلاف الأمامي
Robert G. Coleman, Xiaomin Wang
Cambridge University Press, 1995 - 528 من الصفحات
Recent discoveries of diamond and coesite in the upper crustal rocks of the Earth have drastically changed scientists' ideas concerning the limits of crustal metamorphism. This book provides detailed accounts of the discoveries of diamond and coesite in crustal rocks and provides insights regarding their formation at very high pressures. The formation of these minerals is related to subduction and continental collision and the tectonics, petrological and mineralogical conditions of diamond and coesite formation are each discussed. Written by the leading workers in this exciting field, this book attempts to define an entirely new field of metamorphism - ultrahigh pressure metamorphism (UHPM). In doing so, it explains the formation of ultrahigh pressure minerals and explores new ideas regarding the tectonic setting of this style of metamorphism. This book will be of particular interest to researchers and graduate students of metamorphic petrology and global tectonics.
 

المحتوى

List of contributors vii
1
Experimental and petrogenetic study of UHPM
33
Principal mineralogic indicators of UHP in crustal rocks
96
A case study from the Alps
132
Creation preservation and exhumation of UHPM
159
The role of serpentinite melanges in the unroofing of UHPM
182
Ultrahighpressure metamorphic rocks in the Western
206
HP and UHP eclogites and garnet peridotites in
244
UHPM terrane in east central China X Wang R Zhang
356
A model for the tectonic history of HP and UHPM regions
391
Diamondbearing metamorphic rocks of the Kokchetav
427
Orogenic ultramafic rocks of UHP diamond facies
456
Index
511
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