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用CAP方法研究大同—阳高4.6级地震震源机制

Study on focal mechanism of the Datong-Yanggao earthquake of M 4.6 by the method of CAP

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【作者】 张玲宋美琴韩立波范瑾赵晓云

【Author】 Zhang Ling;Song Meiqin;Han Libo;Fan Jin;Zhao Xiaoyun;Earthquake Administration of Shanxi Province;National Continental Rift Valley Dynamics Observatory of Taiyuan;Institute of Geophyiscs,China Earthquake Administration;

【机构】 山西省地震局太原大陆裂谷动力学国家野外科学观测研究站中国地震局地球物理研究所

【摘要】 利用CAP方法反演2010年4月4日大同—阳高4.6地震震源机制解,结果表明:此次地震为正断兼有斜滑活动,认为节面Ⅱ的走向、倾向及正断走滑特性与震中附近的六楞山山前断裂吻合,其为发震断裂的可能性较大。

【Abstract】 Focal mechanism solution of the Apr.4,2010 Datong-Yanggao earthquake of M 4.6 is inverted by the method of Cap.M_w = 4.5,nodal plane is 89°,39° and —56° for strike,dip and rake angles,respectively.The other nodal plane is 228°,58°,—114°.The estimated foca!depth is about 10 km,for normal with oblique slippery activity.Combined long axis directior of plane of extract position for sequence and fault of the old earthquake zone of the DatongYanggao earthquake of M 6.1,it is considered that the strike,dip and normal with strikeslip characteristic of the nodal plane TJ inosculate the Liulengshan fault near the epicenter,which is probably the fault generating earthquake.

【基金】 山西省地震局科研项目(SBK-1205)
  • 【文献出处】 地震地磁观测与研究 ,Seismological and Geomagnetic Observation and Research , 编辑部邮箱 ,2013年Z1期
  • 【分类号】P315.33
  • 【被引频次】4
  • 【下载频次】19
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