龙门山中段清平叠覆式飞来峰的厘定  

Identification of the Qingping overlapping klippe in the middle Longmen Mountains,China

作　　者：韩建辉[1] 李忠权[2] 王道永[2] 

机构地区：[1]中国石油大学资源与信息学院,北京102249 [2]成都理工大学地球科学学院,成都610059

出　　处：《成都理工大学学报（自然科学版）》2009年第3期305-310,共6页Journal of Chengdu University of Technology: Science & Technology Edition

基　　金：国家自然科学基金资助项目(40573002;40773030;40373005);四川省杰出青年基金资助项目(03ZQ026-046);四川省应用基础研究项目(05JY029-088-2)

摘　　要：以飞来峰构造的角度对龙门山中段的清平飞来峰构造进行详细的野外地质调查和室内综合分析。结果显示其具有勺状的底滑面,与周围地体在地层层序、构造特征上均有很大差异,应归为飞来峰构造,且该飞来峰具有多层叠置的特点。根据其边界断层、物质组成、变形特征等进一步将清平飞来峰划分为五层,是目前发现的龙门山飞来峰带中层数最多的飞来峰。This paper studies the features of the Qingping klippe by field investigation and interior synthetic analyses as viewed from a kllipe. The Qingping klippe has scoop gliding surfaces and is obviously different from the underlying beds in stratigraphic sequences and structural feature. It is an overlapping klippe and can be divided into five layers. It is the klippe with most layers in found the klippe zone of the Longmen Mountains at present.

关 键 词：飞来峰 龙门山 逆冲推覆构造 

分 类 号：P542[天文地球—构造地质学]