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岷县-漳县6.6级地震洞体应变异常特征

史继平 王小娟 翟玮

地震地磁观测与研究Issue(5):59-63,5.
地震地磁观测与研究Issue(5):59-63,5.DOI:10.3969/j.issn.1003-3246.2015.05.011

岷县-漳县6.6级地震洞体应变异常特征

The abnormal change of cave volume strain for Minxian - Zhangxian MS 6.6 earthquake

史继平 1王小娟 1翟玮1

作者信息

  • 1. 中国兰州 730000 甘肃省地震局
  • 折叠

摘要

Abstract

In this paper,the anomalous variation of cave volume strain data at Dangchang Seismic Station is analyzed. The result suggests that the data has recorded the whole process of earthquake deformation. The process is: interseismic deformation,then,preseismic deformation (which include the acceleration period and unstable period),then,coseismic deformation,then, postseismic deformation (which include the post seismic slip and the adjustment),and last, interseismic deformation. The post seismic slip of long duration is extremely rare in our country, so this data is extremely valuable for the study of earthquake gestation process.

关键词

洞体应变/岷县-漳县MS6.6地震/加速变化期/失稳期/震后调整

Key words

cave volume strain/Minxian-Zhangxian MS 6.6 earthquake/accelerated change period/unstable period/adjustment after the earthquake

引用本文复制引用

史继平,王小娟,翟玮..岷县-漳县6.6级地震洞体应变异常特征[J].地震地磁观测与研究,2015,(5):59-63,5.

基金项目

中国地震局监测、预测、科研三结合课题 ()

地震地磁观测与研究

1003-3246

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