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首页|期刊导航|地质学报|芦山Ms7.0地震前龙门山断裂带西南段区域形变特征分析及发震模型探讨

芦山Ms7.0地震前龙门山断裂带西南段区域形变特征分析及发震模型探讨

徐东卓 焦守涛 朱传宝 孙非非 管见 尹海权

地质学报2017,Vol.91Issue(10):2175-2184,10.
地质学报2017,Vol.91Issue(10):2175-2184,10.

芦山Ms7.0地震前龙门山断裂带西南段区域形变特征分析及发震模型探讨

Regional Deformation Characteristics in the Southwestern Segment of Longmen Mountain Fault Zone before Lushan Ms7.0 Earthquake and Possibly Induced Earthquake Model

徐东卓 1焦守涛 2朱传宝 3孙非非 3管见 1尹海权1

作者信息

  • 1. 中国地震局第一监测中心,天津,300180
  • 2. 中山大学地球科学与工程学院,广州,510275
  • 3. 青海省第三地质矿产勘查院,西宁,810029
  • 折叠

摘要

Abstract

The regional deformation characteristics of the southwestern segment of Longmen Mountain Fault Zone before the Lushan Ms7.0 earthquake were analyzed by using the precise re-leveling data in 2010 and 2013.The results indicate that the vertical deformation rate of the Tianquan-Luding area in the southwestern part of the Longmen Mountain Fault Zone was 6~8 mm /a,which was far higher than that of this region before the Wenchuan Ms8.0 earthquake.The Wenchuan Ms8.0 earthquake accelerated accumulation of the Coulomb stress value in the research area before occurrence of Lushan Ms7.0earthquake.The vertical deformation rate of the Ya'an-Mingshan area close to the Sichuan Basin was-3~-6 mm/a.In terms of the rupture zone and aftershock distribution induced by the Lushan earthquake and Wenchuan earthquake,a "seismic gap" between two earthquakes might accelerate stress accumulation.Therefore,monitoring the "seismic gap" and earthquake prediction should be strengthened.

关键词

芦山地震/龙门山断裂带/精密水准/形变分析/发震模型

Key words

Lushan earthquake/Longmen Mountain Fault Zone/Precise re-leveling data/Deformation analysis/Earthquake model

引用本文复制引用

徐东卓,焦守涛,朱传宝,孙非非,管见,尹海权..芦山Ms7.0地震前龙门山断裂带西南段区域形变特征分析及发震模型探讨[J].地质学报,2017,91(10):2175-2184,10.

基金项目

本文为科技部基础性工作项目(编号:2015FY210400)和中国地震局“三结合”项目(编号:CEA-JC/3JH-163704)联合资助的成果. (编号:2015FY210400)

地质学报

OA北大核心CSCDCSTPCD

0001-5717

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