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2013年4月20日四川芦山M7.0级地震介绍
引用本文:刘杰,易桂喜,张致伟,官致君,阮祥,龙锋,杜方.2013年4月20日四川芦山M7.0级地震介绍[J].地球物理学报,2013,56(4):1404-1407.
作者姓名:刘杰  易桂喜  张致伟  官致君  阮祥  龙锋  杜方
作者单位:1. 中国地震台网中心,北京 100045; 2. 四川省地震局,成都 610041
摘    要:2013年4月20日四川芦山M7.0级地震发生在龙门山断裂带南段,震源机制解为逆冲型.震后3天震区已发生3000多次余震,其中M5级余震4次,最大余震是4月21日17时05分芦山、邛崃交界M5.4级地震,余震区长轴约45 km,短轴约20 km.芦山M7.0级地震与2008年5月12日汶川M8.0级地震均位于龙门山断裂带,但汶川地震发生在该断裂带中-北段,两个地震的余震区存在约45 km的间隔,芦山M7.0级地震不是汶川地震的余震,但两者密切相关.

关 键 词:芦山M7.0级地震  汶川地震  龙门山断裂带  
收稿时间:2013-04-23

Introduction to the Lushan,Sichuan M7.0 earthquake on 20 April 2013
LIU Jie,YI Gui-Xi,ZHANG Zhi-Wei,GUAN Zhi-Jun,RUAN Xiang,LONG Feng,DU Fang.Introduction to the Lushan,Sichuan M7.0 earthquake on 20 April 2013[J].Chinese Journal of Geophysics,2013,56(4):1404-1407.
Authors:LIU Jie  YI Gui-Xi  ZHANG Zhi-Wei  GUAN Zhi-Jun  RUAN Xiang  LONG Feng  DU Fang
Institution:1. China Earthquake Networks Center, Beijing 100045, China; 2. Earthquake Administration of Sichuan Province, Chengdu 610041, China
Abstract:The Lushan, Sichuan M7.0 earthquake on 20 April 2013 occurred on the southern segment of the Longmen Shan fault zone. Its focal mechanism is reverse faulting. Over 3000 aftershocks in 3 days after the mainshock have been recorded, of which 4 events are M5 and the maximal aftershock is the M5.4 shock at 17:05 on 21 April, 2013 on the Lushan-Qionglai border. The long axis is about 45 km and the short axis about 20 km of the aftershock area. Both the Lushan M7.0 earthquake and Wenchuan M8.0 earthquake on 12 May, 2008 took place on the Longmen Shan fault zone, and the Wenchuan event occurred on the central-northern segments. There is about 45 km-long interval between the two aftershock areas. The Lushan M7.0 earthquake is not an aftershock of the 2008 Wenchuan M8.0 earthquake, though there is a close relationship between the two events.
Keywords:Lushan M7  0 earthquake  Wenchuan earthquake  Longmen Shan fault zone
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