青海可可西里地区的活动构造与地震  

STUDY ON THE ACTIVE TECTONIC AND EARTHQUAKE IN KEKEXILI AREA OF QINGHAI PROVINCE

作　　者：叶建青[1] 

机构地区：[1]青海省地震局

出　　处：《高原地震》1994年第2期11-23,共13页Plateau Earthquake Research

摘　　要：青海可可西里地区是青藏高原腹地，自有仪器记录以来，共发生Ｍｓ≥６．０级地震８次，是海省中强地震的主要发震场所之一。本文根据对青海可可西里地区活动断裂的野外考察，较为详细地研究了该区五条活动断裂的几何形态、空间分布及动力学特征。对该区地震活动与构造应力场的关系进行了探讨。结果表明：青海可可西里地区的活动断裂为继承性全新世活动断裂，多发育着史前和现代地震破裂形变带，是该区的主要发震断裂。其中乌兰乌拉湖─岗齐曲活动断裂带是现代地震的主要发震断裂，地表出露有１９８８年４月５日唐古拉Ｍｓ＝７．０级地震的破裂形变带，长达９公里。通过对可可西里地区的野外考察，未发现国外报道的１９７３年７月１６日青海可可西里地区火山活动的事实。Kekexili area of Qinghai province is in hinterland of Qinghai-Xizang Plateau, eight earthquakes occurred there since the beginning of recorded earthquake by instrument. It is major one of seismo-genie place of medium-strong earthquake in Qinghai province.Based on the field survey of active fault in Kekexili of Qinghai, the geometric shape. spatial distribution and kinetic characteristics of five active faults was detailed studied,the relationship between seismicity and tectonic stress field was approached in this paper. The results shdw that: the active faults of Kekexili in Qinghai are succession in Holocene and have prehistorical and recent seismic repture deformation zones, are major triggering seismic fault, in it, Wulanwulahu-Gangqiqu active fault is major triggering seismic fault of recent earthquake and has 9km long repture deformation of Tanggula earthquake with Ms=7.0 on April, 5, 1988.Through field survey, the author didn' t find volcanic activity on July, 16, 1973 was reported by abroad.

关 键 词：野外考察 活动构造 地震形变带 可可西里 

分 类 号：P56[天文地球—构造地质学]