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2013年甘肃岷县—漳县M 6.6地震序列精定位研究

梁姗姗 徐志国 杜广宝 刘敬光 张广伟

地震地磁观测与研究2017,Vol.38Issue(2):12-16,5.
地震地磁观测与研究2017,Vol.38Issue(2):12-16,5.DOI:10.3969/j.issn.1003-3246.2017.02.003

2013年甘肃岷县—漳县M 6.6地震序列精定位研究

Precise relocation of Minxian-Zhangxian M 6.6 earthquake sequence in Gansu Province, 2013

梁姗姗 1徐志国 2杜广宝 3刘敬光 1张广伟1

作者信息

  • 1. 中国北京100045 中国地震台网中心
  • 2. 中国北京100085 中国地震局地壳应力研究所地壳动力重点实验室
  • 3. 中国北京100081 国家海洋环境预报中心
  • 折叠

摘要

Abstract

Applying the double-difference algorithm to the Minxian-Zhangxian,mainshock (M 6.6) and its 388 aftershocks after 48 hours,Gansu on July 22 2013,we obtained 350 relocated earthquakes.Our results show that the aftershocks are shown as a shovel-shaped structure with a large northeastward dip extending for over 12 km long along the north-west direction and have an approximately symmetrical distribution about a center of the mainshock.The aftershocks are focused at depths of 4-10 km,but they migrate from about 10 km depth to above 3 km depth and their magnitudes range from 3-4 in a deeper layer to 2-3 in a shallower layer.The aftershocks show clearly a double-layer structure,one of which is at 4-10 km depth,while the other is above 3 km depth.There are few events between these two layers.The shallow earthquake layer could be one of causes that made a strong damage in the event.The vertical cross section of aftershock hypocenters shows a northeast tilt of the fault plane,suggesting that the seismogenic fault of this mainshock could be the Lintan-Diachang fault.

关键词

岷县—漳县主震/余震/双层结构/高倾角/双差定位

Key words

Minxian-Zhangxian earthquake/aftershocks/double-layer structure/large dip/double-difference algorithm

引用本文复制引用

梁姗姗,徐志国,杜广宝,刘敬光,张广伟..2013年甘肃岷县—漳县M 6.6地震序列精定位研究[J].地震地磁观测与研究,2017,38(2):12-16,5.

基金项目

中国地震局地震科技星火计划(项目编号:XH17049Y) (项目编号:XH17049Y)

地震地磁观测与研究

1003-3246

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