大别山南部的低级变质岩:宿松群和张八岭群 LOW-GRADE METAMORPHIC ROCKS IN SOUTHERN DASBIE MT.: THE SU

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大别山南部的低级变质岩:宿松群和张八岭群

LOW-GRADE METAMORPHIC ROCKS IN SOUTHERN DASBIE MT.: THE SUSONG AND ZHANGBALING GROUP

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.

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作 者: 徐树桐 吴维平 陆益群 汪德华 XU Shu-tong WU Wei-ping LU Yi-qu WANG De-hua  
作者单位:安徽省地质调查院.安徽,合肥,230001 
刊 名:安徽地质 
英文刊名:GEOLOGY OF ANHUI 
年,卷(期):2010 20(1) 
分类号:P588.3 
关键词:低级变质岩   宿松群   张八岭群   大别山  
机标关键词:大别山南部低级变质岩宿松群SOUTHERN浅变质岩俯冲造山带晚元古代结晶基底构造单元佛子岭群对应关系大陆边缘沉积不整合梅山北部 
基金项目: 
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