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The Focal Mechanism Solutions of the Ms 8.0 Wenchuan Earthquake in Sichuan on May 12,2008 and Some of Its Aftershocks

机译:2008年5月12日四川汶川8.0级地震的震源机制解及其余震。

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The focal mechanism solutions of the Wenchuan earthquake(Ms8.0)of May 12,2008 and some of its aftershocks occurring up to December 10,2008 are determined with lower semisphere of equal-projection and first motion sign data of P waves from regional and distant stations.The focal mechanism solutions of the Ms8.0 Wenchuan earthquake are:Nodal plane Ⅰ:strike 5°,dip angle 48°,slip angle 39°; Nodal plane Ⅱ: strike 247°,dip angle62°,slip angle 131°; P axis azimuth 309°,plunge 8°,T axis azimuth 208°,plunge 54°,B axis azimuth 44°,plunge 35°.Combining geological tectonics and spatial distribution of aftershocks,nodal plane Ⅱ can be identified as a seismogenic fault.According to focal mechanism solutions,the fault activity that triggered the huge earthquake is reverse thrusting.The main rupture surface is S67°W,basically identical to the fault strike on which the earthquake occurred.The main compression stress P axis is N51°W,which is basically the same as the direction of the regional tectonic stress field.According to the results of focal mechanism solutions of aftershocks,the aftershocks occurring in the southern and northern sections of the Longmenshan fault zone have predominant orientations and are obviously different.For the main shock and the early aftershocks occurring on the southern section of the Longmenshan fault,the rupturing is mainly characterized by reverse-dip slip with some strike-slip,and over time,the aftershocks migrated towards the northern section.The rupturing in the source is mainly characterized by strike-slip with some reverse-dip slips.The stress field is controlled by the main shock stress field in the southern section of the Longmenshan tectonic zone,while it is controlled by the main shock stress field and regional stress field in the northern section of the Longmenshan tectonic zone.
机译:利用等投影下半球和来自地区和太平洋的P波的第一运动标志数据确定2008年5月12日汶川地震(Ms8.0)及其直到2008年12月10日发生的余震的震源机制解。汶川Ms8.0地震的震源机制解为:节点Ⅰ:走向5°,倾角48°,滑动角39°;节点平面Ⅱ:走向247°,倾角62°,滑移角131°; P轴方位角309°,倾角8°,T轴方位角208°,倾角54°,B轴方位角44°,倾角35°。结合余震的地质构造和空间分布,节点Ⅱ可认为是地震成因。根据震源机制解,引发大地震的断层活动是反推力。主破裂面为S67°W,基本与发生地震的断层走向相同。主压应力P轴为N51°W,根据余震的震源机制解结果,龙门山断裂带南,北断层发生的余震具有主要的方向,明显不同。龙门山断裂带南部发生主震和早余震,破裂的主要特征是逆倾滑动和一些走滑,随着时间的推移,余震震源的破裂主要表现为走滑和一些反倾滑。应力场受龙门山构造带南段主震应力场控制,而受控制由龙门山构造带北部的主震应力场和区域应力场组成。

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