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内蒙古地区地壳速度模型在地震定位中的应用

刘芳 宋秀青 张帆 李彬 赵星 刘永梅 王勇 朱元清

地震地磁观测与研究2016,Vol.37Issue(4):27-32,6.
地震地磁观测与研究2016,Vol.37Issue(4):27-32,6.DOI:10.3969/j.issn.1003-3246.2016.04.006

内蒙古地区地壳速度模型在地震定位中的应用

Application of the crust velocity model of Inner Mongolia region in earthquake location

刘芳 1宋秀青 2张帆 1李彬 1赵星 1刘永梅 1王勇 1朱元清2

作者信息

  • 1. 中国呼和浩特010051内蒙古自治区地震局
  • 2. 中国上海200062上海市地震局
  • 折叠

摘要

Abstract

According to random drawing earthquake test in Inner Mongolia between 2009 and April 2014, using Hyposat software, the location residual of the new model is lower. Mean positioning residual obtain with the optimal model is 0.19 s lower and the mean optima-catalog epicenter differential is 1.19 km lower, which shows that the optimal model results is closer to the epicenter catalog results. According to the three dimensional depth distribution, latitude depth according projection and the longitude depth projection, strip shaped gathered around 5 km. The catalog depth scattered between 5 and 10 km, while the optimal model focal depth scattered between 10 and 25 km. It is suggested that the new model is more suitable for seismic observation work in Inner Mongolia network.

关键词

内蒙古地区/2015地壳速度模型/地震定位/定位残差/震中差

Key words

Inner Mongolia region/the 2015 crust model/earthquake location/location residual/epicenter difference

引用本文复制引用

刘芳,宋秀青,张帆,李彬,赵星,刘永梅,王勇,朱元清..内蒙古地区地壳速度模型在地震定位中的应用[J].地震地磁观测与研究,2016,37(4):27-32,6.

基金项目

内蒙古自治区科技计划项目(20130437)、中国地震局地震科技星火项目( XH15008)、中国地震局监测司专项(震源深度核实复测及全国优势深度分布图产出)和中国地震局科技星火项目( XH14012Y)联合资助 ()

地震地磁观测与研究

1003-3246

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