湖北英山-安徽太湖地区构造变形特征  

Deformation Characteristics of Yingshan in Huibei Province and Taihu Area in Anhui Province

作　　者：吴海权[1] 江来利[1] 储东如[1] 刘铭[2] 

机构地区：[1]安徽省地质调查院,安徽合肥230001 [2]山东省鲁南地质工程勘察院,山东兖州272100

出　　处：《山东国土资源》2016年第12期8-13,共6页Shandong Land and Resources

基　　金：国土资源部地质大调查资助项目(200013000108)

摘　　要：湖北英山—安徽太湖地区位于大别山造山带东段,在对区域构造岩石地层调查与分析基础上,确定大别山造山带结构主要为构造-岩片堆叠体,自北向南依次划分为罗田-岳西变质杂岩带、英山-潜山超高压岩片、宿松变质岩片等3个构造岩片,分别对其构造变形特征进行了详细阐述和分析,为进一步研究大别山造山带提供了可靠的构造依据。Yingshan in Hubei province and Taihu area in Anhui province located in east part of Dabie oro- genic belt. On the basis of investigation and analysis of regional tectonic rock stratum, it is determined structures of Dabie orogenic belt are mainly tectonic slices stacked body From the north to the south. It can be divided into Luotian--Yuexi metamorphic complex belt, Yingshan --Qianshan ultra--pressure rocks and Susong metamorphic rocks in turn. Tectonic deformation characteristics have been described and ana- lyzed in detail. It will provide a reliable structural basis for further research of Dabie mountains.

关 键 词：大别山造山带 构造 变形特征 湖北英山--安徽太湖地区 

分 类 号：P315[天文地球—地震学]