SEISMOLOGY AND GEOLOGY ›› 2008, Vol. 30 ›› Issue (2): 359-362.

• Brief Report • Previous Articles     Next Articles

RUPTURE OF THE MS 8.0 WENCHUAN EARTHQUAKE

HE Hong-lin1, SUN Zhao-min2, WANG Shi-yuan3, WANG Ji-qiang2, DONG Shao-peng1   

  1. 1. Institute of Geology, China Earthquake Administration, Beijing 100029, China;
    2. Earthquake Administration of Shandong Province, Jinan 250014, China;
    3. Earthquake Administration of Sichuan Province, Chengdu 100717, China
  • Received:2008-06-10 Revised:2008-06-11 Online:2008-06-20 Published:2009-08-16

汶川MS8.0地震地表破裂带

何宏林1, 孙昭民2, 王世元3, 王纪强2, 董绍鹏1   

  1. 1. 中国地震局地质研究所, 北京, 100029;
    2. 山东省地震局, 济南, 250014;
    3. 四川省地震局, 成都, 100717
  • 作者简介:何宏林,男,1964年生,1985年毕业于北京大学地质系,1988年在中国科学技术大学研究生院获得硕士学位,2000年在东京大学获得博士学位,研究员,主要研究方向为地震地质与构造地貌,电话:86(10)62009125,E-mail:honglinhe123@vip.sina.com.

Abstract: On the 12th of May,2008,a devastating MS 8.0 earthquake struck Wenchuan County,Sichuan Province.The earthquake rupture extends about 200km,and the maximum co-seismic strike-slip displacement and vertical displacement are(4.8±0.2)m and(5±0.2)m,respectively.Only one fault plane(N32°E/NW∠76°)has been found on the southern section of the rupture.The high dip of the fault plane and high angle stria on the fault plane show that the fault is dominated by reverse motion,with a small amount of right-lateral strike-slip component in this segment.

Key words: the MS 8.0 Wenchuan Earthquake, surface rupture zone, co-seismic displacement, vertical fault

摘要: 2008年5月12日14时28分4秒,四川省汶川县发生MS8.0大地震。发震断裂为龙门山断裂带中的映秀-北川断裂。该次地震的地表破裂可分成2条,分别出现在龙门山断裂带中的映秀-北川断裂、彭县-灌县断裂上,前者破裂长度约200km,后者破裂长度约80km。本次地震的最大垂直和右旋水平同震位移出现在都江堰市虹口乡附近的映秀-北川断裂上,分别为(5±0.2)m和(4.8±0.2)m。破裂带南段出露的地表断层产状为N32°E/NW∠76°,其上的侧伏角为S75°~80°W,反映了该次地震在南段以逆冲运动为主,兼有少量的右旋走滑分量。

关键词: 汶川MS8.0地震, 地表破裂带, 同震位移, 逆冲断层

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