汶川地震发震断层破裂触发过程

贺鹏超, 沈正康. 汶川地震发震断层破裂触发过程[J]. 地球物理学报, 2014, 57(10): 3308-3317, doi: 10.6038/cjg20141018
引用本文: 贺鹏超, 沈正康. 汶川地震发震断层破裂触发过程[J]. 地球物理学报, 2014, 57(10): 3308-3317, doi: 10.6038/cjg20141018
HE Peng-Chao, SHEN Zheng-Kang. Rupture triggering process of Wenchuan earthquake seismogenic faults[J]. Chinese Journal of Geophysics (in Chinese), 2014, 57(10): 3308-3317, doi: 10.6038/cjg20141018
Citation: HE Peng-Chao, SHEN Zheng-Kang. Rupture triggering process of Wenchuan earthquake seismogenic faults[J]. Chinese Journal of Geophysics (in Chinese), 2014, 57(10): 3308-3317, doi: 10.6038/cjg20141018

汶川地震发震断层破裂触发过程

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    作者简介:

    贺鹏超, 男, 1989年生, 2011年获北京大学学士学位, 现为北京大学在读博士研究生. E-mail:hepengchaoslg@pku.edu.cn

    通讯作者: 沈正康, 男, 教授, 1990年获美国加州大学洛杉矶分校地球物理博士学位, 主要从事卫星大地测量、地震学和地球动力学等方面的研究. E-mail:zhengkangshen@pku.edu.cn
  • 中图分类号: P315

Rupture triggering process of Wenchuan earthquake seismogenic faults

More Information
  • 2008年汶川大地震造成北川断裂、彭灌断裂、小渔洞断裂等多条断裂的破裂,呈现出复杂的破裂过程. 对此,以往地震学的研究没有对于各个发震断层的破裂先后顺序给出充分论证. 本文计算由于断层破裂在其他断层段上造成库仑应力的变化,根据其相互触发关系确定断层可能的破裂顺序. 结果表明,各断裂带可能的发震顺序为:主震在北川断裂南端(小渔洞断裂以南的北川断裂虹口段)起始,造成北川断裂的后续段落龙门山镇—清平段和彭灌断裂同时破裂,进而触发小渔洞断裂发生破裂.
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出版历程
收稿日期:  2013-10-30
修回日期:  2014-07-16
上线日期:  2014-10-20

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