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云南地壳形变与丽江7.0级地震
引用本文:张兴华,宋金玲.云南地壳形变与丽江7.0级地震[J].地震研究,1997,20(1):72-82.
作者姓名:张兴华  宋金玲
作者单位:云南省地震局
摘    要:本利用滇西、滇中地区大地垂直形变和跨断层短水准、短基线的监测资料进行综合分析论证,其结果表明:1996年2月滇西丽江7.0级地震前,该区应力场方向自1990年以来产生了由北东-北西的转变,震源区出现高达109mm的垂直差异运动1993-1996年有75%的断层形变测点相继出现不同程度的中期、短期和临震异常。大地垂直形变与断层形变的共性演变特性,为强震的预测提供了一个较好的震例。

关 键 词:云南  地壳变形  地震  震级

CRUSTAL DEFORMATION AND THE M 7 0 LIJIANG EARTHQUAKE IN YUNNAN
Zhang Xinhua,Song Jinlin,Wan Qingwei and Shao Desheng.CRUSTAL DEFORMATION AND THE M 7 0 LIJIANG EARTHQUAKE IN YUNNAN[J].Journal of Seismological Research,1997,20(1):72-82.
Authors:Zhang Xinhua  Song Jinlin  Wan Qingwei and Shao Desheng
Abstract:Comprehensive analysis and demonstration have been made in this paper by using the data from the geodetic vertical deformation, fault-crossing short-leveling and short-base line surveys in middle and western Yunnan. The results show that before the M 7 7 Lijiang earthquake in west Yunnan on Feb.3, 1996, the direction of stressfield in this region has shifted from NE to NW and vertical differential motion come up to 109 mm since 1990 in the focal region; medium and short term and impending anomalies appeared to varying degrees at 75% of fault deformation observation poinsts from 1993 to 1996. The common evolution characteristics of geodetic vertical defromation and fault deformation give a good example for strong earthquake prediction.
Keywords:Vertical deformation  stress-strain relation  stress measurement  M 7  0 Lijiang earthquake  Yunnan  
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