SEISMOGENIC STRUCTURES ASSOCIATED WITH THE 20 APRIL 2013 MS 7.0 LUSHAN EARTHQUAKE, SICHUAN PROVINCE

doi:10.3969/j.issn.0253-4967.2013.03.020

SEISMOLOGY AND GEOLOGY ›› 2013, Vol. 35 ›› Issue (3): 671-683.DOI: 10.3969/j.issn.0253-4967.2013.03.020

SEISMOGENIC STRUCTURES ASSOCIATED WITH THE 20 APRIL 2013 M_S 7.0 LUSHAN EARTHQUAKE, SICHUAN PROVINCE

LI Chuan-you¹, XU Xi-wei¹, GAN Wei-jun², WEN Xue-ze^3,4, ZHENG Wen-jun², WEI Zhan-yu¹, XU Chong¹, TAN Xi-bin¹, CHEN Gui-hua¹, LIANG Ming-jian⁴, LI Xin-nan¹

1. Key Laboratory of Active Tectonics and Volcano, Institute of Geology, China Earthquake Administration, Beijing 100029, China;
2. State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China;
3. Key Laboratory of Earthquake Science, Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, China;
4. Earthquake Administration of Sichuan Province, Chengdu 610041, China

Received:2013-08-25 Revised:2013-09-11 Online:2013-09-30 Published:2013-10-12

四川省芦山M_S7.0地震发震构造分析

李传友¹, 徐锡伟¹, 甘卫军², 闻学泽^3,4, 郑文俊², 魏占玉¹, 许冲¹, 谭锡斌¹, 陈桂华¹, 梁明剑⁴, 李新男¹

1. 中国地震局地质研究所, 活动构造与火山重点实验室, 北京 100029;
2. 中国地震局地质研究所, 地震动力学国家重点实验室, 北京 100029;
3. 中国地震局地震预测研究所, 地震预测重点实验室, 北京 100036;
4. 四川省地震局, 成都 610041

作者简介:李传友,男,1971年生,中国地震局地质研究所构造地质专业博士学位,研究员,主要研究方向为活动构造,电话:010-62009121,E-mail:chuanyou@ies.ac.cn。
基金资助:
国家自然科学基金(41172322)和中国地震局地质研究所基本科研业务专项(IGCEA1114)共同资助

Abstract

Abstract:

The April 20,2013,M_S 7.0 Lushan earthquake occurred along the southwestern part of the Longmen Shan Fault zone. Tectonics around the epicenter area is complicated and several NE-trending faults are developed. Focal mechanisms of the main shock and inversions from finite fault model suggest that the earthquake occurred on a northeast-trending,moderately dipping reverse fault,which is consistent with the strike and slip of the Longmen Shan Fault zone. NE-trending ground fissures and soil liquefaction along the fissures,heavy landslides along the Dachuan-Shuangshi and Xinkaidian Faults were observed during the field investigations. No surface ruptures were found in the field work. GPS data indicate that the fault on which this earthquake occurred is a fault east of or near the Lushan county and the earthquake also triggered slip on the fault west of the Lushan county. Field observations,GPS data,focal fault plane,focal depth,and distribution of the aftershocks suggest, that the seismogenic structure associated with the M_S 7.0 Lushan earthquake is the décollement beneath the folds of the eastern Longmen Shan. Slip along this decollement generated the earthquake,and also triggered the slip along the Dachuan-Shuangshi and Xinkaidian Faults.

Key words: Lushan M_S 7.0 earthquake, seismogenic structures, the Longmen Shan Fault zone, the dé, collement of the eastern Longmenshan

摘要：

2013年4月20日的芦山 "4·20"M_S7.0地震发生在龙门山断裂带西南段,震中地区分布多条NE向断裂,构造较为复杂。这次地震震源机制解显示为逆冲型地震,破裂面为NE走向,与龙门山断裂带的运动性质和走向一致。地表调查只在大川-双石断裂(前山断裂)和新开店断裂(大邑断裂南段)发现局部分布的NE向地表裂缝、沿地表裂缝分布的喷砂冒水和砂土液化,不规则的边坡开裂等地表变形,以及断裂沿线较严重的滑坡崩塌和房屋破坏。野外调查没有发现明显的地震地表破裂。GPS测量结果显示,此次地震的发震断裂位于芦山县城附近或其以东,而芦山西侧的断裂也可能参与了部分活动。根据野外地质调查、GPS观测、震源机制解、震源深度、余震分布等结果综合判定,芦山7.0级地震的主要发震构造是芦山之下、大川-双石断裂和新开店断裂之间的龙门山前缘滑脱带。此滑脱带在该段的运动导致了这次地震的发生,并可能带动了它上面的大川-双石和新开店等断裂的活动。

关键词: 芦山7.0级地震, 发震构造, 龙门山断裂带, 龙门山前缘滑脱带

CLC Number:

P315.5

LI Chuan-you, XU Xi-wei, GAN Wei-jun, WEN Xue-ze, ZHENG Wen-jun, WEI Zhan-yu, XU Chong, TAN Xi-bin, CHEN Gui-hua, LIANG Ming-jian, LI Xin-nan. SEISMOGENIC STRUCTURES ASSOCIATED WITH THE 20 APRIL 2013 M_S 7.0 LUSHAN EARTHQUAKE, SICHUAN PROVINCE[J]. SEISMOLOGY AND GEOLOGY, 2013, 35(3): 671-683.

李传友, 徐锡伟, 甘卫军, 闻学泽, 郑文俊, 魏占玉, 许冲, 谭锡斌, 陈桂华, 梁明剑, 李新男. 四川省芦山M_S7.0地震发震构造分析[J]. 地震地质, 2013, 35(3): 671-683.

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SEISMOGENIC STRUCTURES ASSOCIATED WITH THE 20 APRIL 2013 M_S 7.0 LUSHAN EARTHQUAKE, SICHUAN PROVINCE

四川省芦山M_S7.0地震发震构造分析

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SEISMOGENIC STRUCTURES ASSOCIATED WITH THE 20 APRIL 2013 MS 7.0 LUSHAN EARTHQUAKE, SICHUAN PROVINCE

四川省芦山MS7.0地震发震构造分析

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SEISMOGENIC STRUCTURES ASSOCIATED WITH THE 20 APRIL 2013 M_S 7.0 LUSHAN EARTHQUAKE, SICHUAN PROVINCE

四川省芦山M_S7.0地震发震构造分析