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利用FOCMEC方法反演2011年江西瑞昌与湖北阳新交界M_S4.6地震的震源机制解
引用本文:包秀敏,梁一婧,顾强强.利用FOCMEC方法反演2011年江西瑞昌与湖北阳新交界M_S4.6地震的震源机制解[J].防灾减灾学报,2012,28(3):48-52.
作者姓名:包秀敏  梁一婧  顾强强
作者单位:沈阳地震台,辽宁沈阳,110161
摘    要:利用FOCMEC方法反演了2011年9月10日江西瑞昌与湖北阳新交界MS4.6地震的震源机制解。反演结果为:节面I的走向304°,倾角76°,滑动角4°;节面Ⅱ的走向213°,倾角86°,滑动角165°;P轴的方位角、倾角分别为260°、7°;T轴的方位角、倾角分别为168°、13°;B轴的方位角、倾角分别为19°、75°。其中节面Ⅱ的走向和活动性质与震中附近的郯庐断裂带的分支断裂——池河—西山驿断裂较为接近。分析认为NNE向的池河—西山驿断裂可能是瑞昌—阳新MS4.6地震的发震构造。

关 键 词:震源机制解  FOCMEC方法  江西瑞昌与湖北阳新交界MS4.6地震  郯庐断裂带

THE FOCAL MECHANISM OF 2011 Ms4.6 EARTHQUAKE IN THE BORDER REGION OF JIANGXI RUICHANG AND HUBEI YANGXIN INVERSED BY FOCMEC METHOD
BAO Xiu-min,LIANG Yi-jing,GU Qiang-qiang.THE FOCAL MECHANISM OF 2011 Ms4.6 EARTHQUAKE IN THE BORDER REGION OF JIANGXI RUICHANG AND HUBEI YANGXIN INVERSED BY FOCMEC METHOD[J].Seismological Research of Northeast China,2012,28(3):48-52.
Authors:BAO Xiu-min  LIANG Yi-jing  GU Qiang-qiang
Affiliation:(Shenyang Seismic Station, Liaoning Shenyang 110161, China)
Abstract:The focal mechanism of 2011 Ms4.6 earthquake in the border region of Jiangxi Ruichang and Hubei Yangxin has been inversed by using FOCMEC method. The result is as follows: the strike, dip and rake angles of nodal plane I are 304°, 76° and 4°. And those of nodal plane 11 are 213°, 86°and 165°. The azimuth and dip angle are 260°and 7° for P axis , 168° and 13° for T axis , 19° and 75° for B axis. The strike angle and activity characteristic are in accord with the branch fault of Tan-Lu fault zone, Chihe-Xishan Yi fault, which is near the epicenter. So it is analyzed that NNE trend Chihe-Xishan Yi fault may be the causative fault of Ruichang-Yangxin Ms4.6 earthquake.
Keywords:focal mechanism solution  FOCMEC method  Ms4  6 earthquake in the border region of Jiangxi Ruichang and Hubei Yangxin  Tan-Lu fault zone
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