措勤地区活动断层构造特征  

TECTONIC CHARACTERISTICS OF THE ACTIVE FAULTS IN CUOQIN AREA

作　　者：张中言[1] 刘登忠[1] 范强[1] 段元彬[1] 

机构地区：[1]成都理工大学地球科学学院,四川成都610059

出　　处：《高原地震》2008年第4期54-58,68,共6页Plateau Earthquake Research

摘　　要：青藏高原自然环境恶劣,地震台网分布稀疏,基于ETM数据,对措勤地区活动断层构造进行了解译,并建立了活动断层构造框架。通过分析活动断层与地震活动性的关系,指出措勤地区活动断层的活动性对青藏高原地震研究有着重要的意义。The natural environment of Qinghai - Xizang Plateau is badly, and the distribution of seismological network is rarely. On the base of ETM data, the structures of active faults in Cuoqin area are deerypted and built up the tectonic frame of these faults. The relationship between the active faults and the seismicity is analyzed and pointed out that the tectonic fault activity referred to earthquake research in the plateau.

关 键 词：措勤 ETM 活动断层 

分 类 号：P315.2[天文地球—地震学]