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几种常用地方震相对天然地震震源深度测定的误差解析分析及数值对比

刘双庆 梁建宏 朱元清 于俊谊 谢静

地震学报2018,Vol.40Issue(2):143-159,17.
地震学报2018,Vol.40Issue(2):143-159,17.DOI:10.11939/jass.20170106

几种常用地方震相对天然地震震源深度测定的误差解析分析及数值对比

Natural hypocentral depth error calculated from some conventional local seismic phases by analytic method and numerical simulation

刘双庆 1梁建宏 2朱元清 3于俊谊 4谢静1

作者信息

  • 1. 中国 天津 300201 天津市地震局
  • 2. 中国 北京 100045 中国地震台网中心
  • 3. 中国 上海 200062 上海市地震局
  • 4. 中国 杭州 310013 浙江省地震局
  • 折叠

摘要

Abstract

In this paper,both analytic and numerical simulation methods were used to discuss the focal depth error resulted from the local seismic phases of Pg,Sg,PmP,Pn,sPL.The result shows the two above methods produced very close error estimation.For the epicenter in the upper crust,on the condition of travel time error within 0.1 s,in order to ensure the depth error is less than 3 km,we should select these direct wave phases recorded within epicentral distance of 30 km to locate.If the travel time error is up to 0.2 s,we should select these direct wave phases within 20 km to locate on the above same condition.When the hypocenter in the lower crust,the limit of epicentral distance could be broaden a bit.As the epicentral distance or travel time error becomes larger,the error of depth location becomes practically several fold increase.Whereas,the seismic phases of PmP,Pn,sPL can make a better error constrain when the hypocenter in the upper crust,and without an obvious enlarging effect on error as the epicentral distance increases.For these three mentioned phases,they also can ensure the depth error within 3.5 km when travel time error is set within 0.1 s and epicentral distance is less than 90 km.Furthermore,by the chessboard mode we analyzed the quantitative effect of travel time resulted from the velocity disturbance.And based on the capital seismic network,we analyzed the improvement of depth location after adding head wave phases.The above analyses result show that,within 2% velocity disturbance and without simultaneously too large or too small velocity deviation for the lower crust and Moho interface,adding head wave phases can effectively produce a reliable focal depth within 3 km,and also produce a more homogeneity result than only direct wave phases used.

关键词

深度震相/震源深度/误差分析/地震定位

Key words

depth phase/focal depth/error analysis/earthquake location

分类

天文与地球科学

引用本文复制引用

刘双庆,梁建宏,朱元清,于俊谊,谢静..几种常用地方震相对天然地震震源深度测定的误差解析分析及数值对比[J].地震学报,2018,40(2):143-159,17.

基金项目

中国地震局地震科技星火计划(XH17003Y)、经常性项目“国家自动速报中心(CSN/GSN)运维及系统优化”和中国地震局震情跟踪项目(2017010128)联合资助. (XH17003Y)

地震学报

OA北大核心CSCDCSTPCD

0253-3782

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