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WFSD地应力台应变特征及其同震效应分析——以日本Mw9.0级特大地震为例

彭华 马秀敏 姜景捷 彭立国

地质力学学报2011,Vol.17Issue(1):1-14,14.
地质力学学报2011,Vol.17Issue(1):1-14,14.

WFSD地应力台应变特征及其同震效应分析——以日本Mw9.0级特大地震为例

STRAIN CHARACTERISTICS OF WFSD STRESS STATIONS AND ITS CO-SEISMIC EFFECTS ANALYSIS: A CASE STUDY UPON Mw 9.0 EARTHQUAKE IN JAPAN

彭华 1马秀敏 1姜景捷 1彭立国2

作者信息

  • 1. 国土资源部 新构造运动与地质灾害重点实验室,北京100081;中国地质科学院 地质力学研究所,北京100081
  • 2. 国土资源部 新构造运动与地质灾害重点实验室,北京100081
  • 折叠

摘要

Abstract

The Mw9. 0 earthquake occurred in the northeastern Sea of Japan, on March 11, 2011. The volume strain meter in Wenchuan earthquake Fault Scientific Drilling ( WFSD) recorded a complete response waveform at Hanzhong Prefecture, Shaanxi Province. By analyzing acquired data, some issues are studied and discussed by authors that including co-seismic changes of the whole process of Mw9. 0 mega-earthquake in Japan, the abnormal strain changes of solid tide prior to that earthquake and after, and the emerging process of that earthquake. Per this paper, the strain anomalies of the Mw9. 0 earthquake in Japan are analyzed in order to contribute to better forecast earthquake trends in China the future.

关键词

日本Mw9.0级特大地震/WFSD/体应变观测/应变特征/同震效应

Key words

Mw 9.0 large earthquake in Japan/ Wenchuan earthquake Fault Science Drilling (WFSD) / volume strain observations/ strain characteristics/ co-seismic effects

分类

天文与地球科学

引用本文复制引用

彭华,马秀敏,姜景捷,彭立国..WFSD地应力台应变特征及其同震效应分析——以日本Mw9.0级特大地震为例[J].地质力学学报,2011,17(1):1-14,14.

基金项目

科技支撑计划项目“汶川地震断裂带科学钻探”-“井中科学探测”课题、“地震断裂带的应力环境、应变能的分布及其与地震关系”课题和地调项目(1212010916064)联合资助. (1212010916064)

地质力学学报

OACSCDCSTPCD

1006-6616

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