| 北部湾6．1、6．2级地震发震构造探讨 |
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| 引用本文： | 任镇寰,钟贻军,罗振暖.北部湾6．1、6．2级地震发震构造探讨[J].华南地震,1996,16(3):89-95. |
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| 作者姓名： | 任镇寰 钟贻军 罗振暖 |
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| 作者单位： | 广东省地震局 |
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| 摘 要： | 北部湾６．１、６．２级地震震源位于北部湾盆地的东部，构造上处于盆地内部ＮＥＥ向的次一级企西凸起与乌石断陷的交界地带，发震断裂主破裂是ＮＥＥ向的北部湾－珠江口外断裂，ＮＷ向的临高断裂可能也参加了活动。
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| 关 键 词： | 发震断裂，地球物理场，断层活动性，北部湾地震 |
DISCUSSION OF SEISMOGENIC STRUCTURE OF THE M_s6.1 and M_s6.2 EARTHQUAKES IN BEIBUWAN |
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| Ren Zhenhuan,Zhong Yijun, Luo Zhennuan.DISCUSSION OF SEISMOGENIC STRUCTURE OF THE M_s6.1 and M_s6.2 EARTHQUAKES IN BEIBUWAN[J].South China Journal of Seismology,1996,16(3):89-95. |
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| Authors: | Ren Zhenhuan Zhong Yijun Luo Zhennuan |
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| Abstract: | The Beibuwan earthquake sources of Ms6.1 and Ms6.2 were located in the intersecting site of the subtectonic Qixi embossment of NEE direction and Wushi depression in eastern Beibuwan basin.The main seismogenic fault is the fault of Beibuwan-outside Pearl myer mouth,and another one maybe is Linggao fault in direction of NW. |
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| Keywords: | Triggering seismic fault Geophysical field Fault activity Beibuwan earthquake |
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