Plurifacial alpine metamorphism in the eastern Betic Cordilleras (SE Spain), with special reference to the genesis of the glaucophane
作者： W. P. De Roever , H. J. Nijhuis
DOI: 10.1007/BF02040754
关键词:
摘要: Rocks metamorphosed in two or more different facies are not necessarily polymetamorphic and termed plurifacial rocks. The following age sequence of metamorphic alpine is reported: (1) glaucophane-schist facies; (2) albite-epidote-amphibolite (S) almandine-amphibolite facies. There was a transition from kinematic to static conditions. metamorphism described seems have proceeded under pile overthrust sheets. change part due considerable rise the temperature.
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