| 1994年台湾海峡7.3级地震发震断层的地震学证据 |
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| 引用本文： | 彭美凤,周峥嵘.1994年台湾海峡7.3级地震发震断层的地震学证据[J].华南地震,2000,20(3):9-13. |
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| 作者姓名： | 彭美凤 周峥嵘 |
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| 作者单位： | 福建省地震局,福建,福州,350003 |
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| 摘 要： | 通过地震学观测资料的分析和研究，并综合其他作者的研究成果，论证了台湾海峡１９９４年７．３级地震发震断层的主破裂面走向应为北西向，地震的发生是由分布于该区域的巴士系构造活动所致。
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| 关 键 词： | 地震断层 断层走向 震源机制 应力场 |
Seismological evidence of seismogenic fault of the M 7.3 Taiwan Strait earthquake |
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| PENG Mei-feng,ZHOU Zheng-rong.Seismological evidence of seismogenic fault of the M 7.3 Taiwan Strait earthquake[J].South China Journal of Seismology,2000,20(3):9-13. |
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| Authors: | PENG Mei-feng ZHOU Zheng-rong |
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| Abstract: | In this paper, the authors proved that the strike of the main fractured surface of the M 7 3 Taiwan Strait earthquake occurred in September 16,1994 must be NW by analyzing the seismic observation data and integrating the research results of other researchers. The authors think that the M 7 3 earfhquake is caused by the activity of the Bashi system tectonic which distributed in this area. |
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| Keywords: | seismic fault fault trend focal mechanism stress field Taiwan Strait earthquake |
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