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大别山南部的低级变质岩:宿松群和张八岭群
引用本文:徐树桐,吴维平,陆益群,汪德华.大别山南部的低级变质岩:宿松群和张八岭群[J].安徽地质,2010,20(1):5-13.
作者姓名:徐树桐  吴维平  陆益群  汪德华
作者单位:安徽省地质调查院.安徽,合肥,230001;安徽省地质调查院.安徽,合肥,230001;安徽省地质调查院.安徽,合肥,230001;安徽省地质调查院.安徽,合肥,230001
基金项目:安徽省地质科学研究所大别山项目;国家自然科学基金项目(40542012);安徽省国土资源厅、安徽省地质矿产勘查局基金匹配项目的支持
摘    要:大别山南部的浅变质岩指宿松群和张八岭群。前者为扬子大陆被动边缘沉积,不整合在扬子大陆晚元古代的结晶基底之上,后者为古大别洋的洋壳,它和北部浅变质岩佛子岭群和梅山群一起,与洋壳俯冲造山带主要构造单元有良好的对应关系。

关 键 词:低级变质岩  宿松群  张八岭群  大别山

LOW-GRADE METAMORPHIC ROCKS IN SOUTHERN DASBIE MT.: THE SUSONG AND ZHANGBALING GROUP
XU Shu-tong,WU Wei-ping,LU Yi-qu,WANG De-hua.LOW-GRADE METAMORPHIC ROCKS IN SOUTHERN DASBIE MT.: THE SUSONG AND ZHANGBALING GROUP[J].Geology of Anhui,2010,20(1):5-13.
Authors:XU Shu-tong  WU Wei-ping  LU Yi-qu  WANG De-hua
Institution:XU Shu-tong,WU Wei-ping,LU Yi-qu,WANG De-hua(Anhui Institute of Geological Survey,Hefei,Anhui 230001,China)
Abstract:The low-grade metamorphic rocks in southern Dabie Mt.refer to Susong and Zhangbaling Groups.The Susong Group is a sequence of the Yangtze passive continental sediments,which unconformably overlies the crystalline basement of the Yangtze craton-the Dabie complex.The Zhangbaling Group is documented to be the oceanic crust of ancient Dabie Ocean plate,which together with the shallow metamorphic rocks in northern Dabie Mountains fairly consists with the major tectonic elements of a subduction orogen.
Keywords:Dabie Mt    low-grade metamorofic rocks  Susong Group  Zhangbaling Group  
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