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北部湾地震的震源机制及地震地质条件
引用本文:尹克坚,吴时平.北部湾地震的震源机制及地震地质条件[J].华南地震,1996,16(3):77-81.
作者姓名:尹克坚  吴时平
作者单位:广西壮族自治区地震局
摘    要:对北部湾地震的震源机制解和地震地质条件进行了详细分析,认为靖西-崇左断裂带过震中的北北西向断层为发震断裂,四会-吴川断裂带过震中的北东东向断层为控震构造,震源构造应力场的主压应力方向为北西-南东向,发震断层的活动方式既有垂直差异运动又有走滑运动。

关 键 词:震源机制  震源模式  北部湾地震  地震地质

FOCAL MECHANISM AND SEISMIC GEOLOGIC CONDITIONS OF THE BEIBUWAN EARTHQUAKES
Yin Kejian,Wu Shiping,Wang Lin.FOCAL MECHANISM AND SEISMIC GEOLOGIC CONDITIONS OF THE BEIBUWAN EARTHQUAKES[J].South China Journal of Seismology,1996,16(3):77-81.
Authors:Yin Kejian  Wu Shiping  Wang Lin
Abstract:The focal mechanism solution and seismic geologic conditions of the Beibuwan earthquakes are discussed.The fault which belongs to Jingxi-Chongzuo fault zone in NW-SE direction and crosses the epicenter is the seismogenic fault.The fault which belongs to Sihui-Wuchuan fault zone in NE-SW direction and crosses the epicenter must have some effects on this seismic sequence.The main pressure direction of the focal stress field is in NW-SE direction.The Beibuwan basin and the fault in and around it inherit the past active model still now.
Keywords:Focal mechanism  Seismogenic fracture  Seismic source mode  Stress field  Beibuqan earthguake
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