昆仑山口西Ms8.1地震前地下流体的远场异常及其意义  

Remote anomalies of subsurface fluid before the Ms8.1 earthquake in west of Kunlun Mountain mouth and their significance

作　　者：车用太[1] 谷元珠[1] 鱼金子[1] 刘五洲[1] 

机构地区：[1]中国地震局地质研究所,北京100029

出　　处：《地震》2002年第4期106-113,共8页Earthquake

摘　　要：简要介绍了2001年11月14日昆仑山口西MS8.1级地震前在河北、陕西、四川、青海、新疆等距震中几百至几千公里之外记录到的地下流体的远场异常(场兆或远兆),并以此为基础讨论了地震孕育的理论与地震预测的科学思路等问题。The paper briefly introduces the remote anomalies (field precursors or remote precursors) that recorded at such places as Hebei, Shaanxi, Sichuan, Qinghai and Xinjiang regions, which are hundreds to thousands kilometers away from the epicenter of the MS8.1 earthquake of west of Kunlun Mountain mouth. Based on the information concerning the earthquake such problems as seismic evolution theory and scientific though of earthquake predication are discussed.

关 键 词：地下流体 运动异常 昆仑山 油田 地震前兆 震源机制解 

分 类 号：P315.723[天文地球—地震学]