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广西灵山地区深部断裂系统的重力资料解释
引用本文:任镇寰,李健梅,乔计花,宫会玲.广西灵山地区深部断裂系统的重力资料解释[J].华南地震,2012(2):1-8.
作者姓名:任镇寰  李健梅  乔计花  宫会玲
作者单位:广东省地震局;中国地震局地震监测与减灾技术重点实验室;广东省地震预警与重大工程安全诊断重点实验室(筹);中国地质调查局发展研究中心
摘    要:采用重力资料系统处理,确认广西灵山地区深部存在近EW向、NW向、NE向三组断裂,它们的深度均可达到40 km,近EW、NW向断裂的强烈活动是1936年灵山63/4级地震发生的主要原因。

关 键 词:重力资料处理  深部断裂  灵山地区

Interpretation of Gravity Data of Deep Fault System in Lingshan Region of Guangxi
REN Zhenhuan,LI Jianmei,QIAO Jihua,GONG Huiling.Interpretation of Gravity Data of Deep Fault System in Lingshan Region of Guangxi[J].South China Journal of Seismology,2012(2):1-8.
Authors:REN Zhenhuan  LI Jianmei  QIAO Jihua  GONG Huiling
Institution:1,2,3(1.Earthquake Administration of Guangdong Province,Guangzhou 510070,China;2.Key laboratory of Earthquake Monitoring and Disaster Mitigation Technology,CEA,Guangzhou 510070,China;3.Key Laboratory of Guangdong Province Earthquake Early Warning and Safety Diagnosis of Major Projects,Guangzhou 510070,China;4.Development Research Center,China Geological Survey Bureau,Beijing 100037,China)
Abstract:Using the processing system of gravity data,this paper shows the existance of three group faults with direction of EW,NW and NE in deep area in Lingshan region of Guangxi.The depth of the three faults can be up to 40 km.The strong activities of EW and NW faults is the major reason of the earthquake with M=63/4 occurred in 1936.
Keywords:Processing of gravity data  Deep faults  Lingshan region
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