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利用连续GPS资料分析芦山7.0级地震区域地壳变形特征

丁晓光 闫伟 张艺 苏利娜 张永奇

灾害学Issue(1):56-62,7.
灾害学Issue(1):56-62,7.DOI:10.3969/j.issn.1000-811X.2015.01.012

利用连续GPS资料分析芦山7.0级地震区域地壳变形特征

Analysis on Deformation Characteristics of the Regional Crust in Lushan M7.0 Earthquake by Continuous GPS Observation Data

丁晓光 1闫伟 2张艺 3苏利娜 1张永奇1

作者信息

  • 1. 陕西省地震局,陕西 西安710068
  • 2. 中国地震局地质研究所,北京100029
  • 3. 中国地震台网中心,北京100045
  • 折叠

摘要

Abstract

In April 20th,201 3,an earthquake attacked the region of Lushan,Sichuan province in the south-ern Longmen mountains fault zone,and caused serious earthquake disaster and secondary hazards.In order to re-search the seismic crustal deformation characteristics,GPS continuous data in 201 0 -201 3 from the CMONOC a-round the epicenter of Lushan earthquake is used,the regional horizontal velocity and vertical deformation are cal-culated,and the coseismic displacement of the station near the epicenter is obtained.Based on the station baselines and strain parameter time series,the regional crustal deformation and strain accumulation background are re-searched;further analysis with the block information separation method shown that the abnormal deformation may exist before the earthquake.The main results got in this paper include:the earthquake region is in the block extru-sion “shunt”zone,and the crustal horizontal movement is small.In the second half of 201 2,a trend of deviation from the original motion was shown by the baseline of QHBM-SCSN and QHBM-SCXJ.Results of deformation sepa-rated from the time series of SCXJ station also showed that,the N and E component of the internal strain contribu-tion had a curve-transition phenomenon.

关键词

芦山7.0级地震/连续GPS数据/地壳运动/应变/时间序列

Key words

Lushan M7.0 earthquake/GPS continuous data/crustal movement/strain/time-series

分类

天文与地球科学

引用本文复制引用

丁晓光,闫伟,张艺,苏利娜,张永奇..利用连续GPS资料分析芦山7.0级地震区域地壳变形特征[J].灾害学,2015,(1):56-62,7.

基金项目

国家“十二五”科技支撑计划(2012BAK19B02);中国地震局地震行业专项 ()

灾害学

OACSCDCSTPCD

1000-811X

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