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北部湾地震的震源机制及地震地质条件
FOCAL MECHANISM AND SEISMIC GEOLOGIC CONDITIONS OF THE BEIBUWAN EARTHQUAKES
【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。
【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.
【关键词】 震源机制;
发震断裂;
震源模式;
应力场;
北部湾地震;
【Key words】 Focal mechanism; Seismogenic fracture; Seismic source mode; Stress field; Beibuqan earthguake;
【Key words】 Focal mechanism; Seismogenic fracture; Seismic source mode; Stress field; Beibuqan earthguake;
- 【文献出处】 华南地震 ,SOUTH CHINA JOURNAL OF SEISMOLOGY , 编辑部邮箱 ,1996年03期
- 【分类号】P315.3
- 【被引频次】14
- 【下载频次】171