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《长春地质学院学报》 1991-03
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COEXISTENCE OF BLUESCHIST AND GREENSCHIST-NEW EVIDENCE FOR TECTONIC EVOLUTION OF THE LONGJIANG SUITES

Zhang Xingzhou Zhang Yuanhou(Department of Geology)  
The metamorphism-deformation relationships of rocks and minerals and their chemical characteristics indicate that coexistence of blueschist and greenschist in the Longjiang Suites do not result from single metamorphic event, but from the tectonism and discontinuous metamorphism. event,but from the overprint of tectonism and discontinuous metamorphism.By late influence of tectonic movement, early formed blueschists under high-pressure and high-oxygen fugacity were transformed into high geoth-ermal gradient deformation belt, and suffered ductile deformation and greenschist facies metamorphism. In the process of the deformation metamorphism,transition of sodic amphibole to sodic-calc amphibole represents a dis-continuously increasing temperature, and that of sodic-calc amphibole to calc amphibole reveals a continuously increasing temperature.
【CateGory Index】: P588.3, P574.2
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