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《GEOLOGY OF ANHUI》 1995-03
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STUDY ON THE ULTRA─HIGH PRESSURE METAMORPHIC MINERALS,SUSONG,ANHUI

Jing Yanren;Tang Jiafu;Gao Tianshan;Hou Mingjin(Regional Geological Survey of Anhui )  
The paper on basis of identification of many tests first reports the existence of high─Pmetamorphic topaz,lazulite l garnet,hornblende and coesite in the Susong area. The aluminum─rich argillite(broadly called white schist by Schreger) marked with topaz is renamed yellow schist by reference to the nomenclature of blue schist and green schist.Study indicates that the Susong area is a ultra─high pressure metamorphic belt with enough mineralogical evidences.
【CateGory Index】: P588.3
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1 TANG Jia- fu1, LI Hui- min2, QIAN Cun- chao1,GAO Tian- shan1(1Anhui Academy of Geological Survey,Hefei 230001,China; 2 Tianjin Institute of Geology and Mineral Resources,Tianjin 300170,China);THE GEOLOGICAL AND CHRONOLOGIC BASIS FOR THE FORMATION TIME OF ECLOGITES IN THE DABIE MTS AND SULU AREA[J];GEOLOGY OF ANHUI;2000-03
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