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Regional Stress Field and Seismic Dynamics Along the Border Zone Between Fujian, Guangdong and Jiangxi Provinces
引用本文:LüJian,Zhang Fuping,Hu Cui''e,Wang Zhiguo,Huang Shuangfeng,Xie Xüiqiang.Regional Stress Field and Seismic Dynamics Along the Border Zone Between Fujian, Guangdong and Jiangxi Provinces[J].中国地震研究,2003,17(2):134-144.
作者姓名:LüJian  Zhang Fuping  Hu Cui'e  Wang Zhiguo  Huang Shuangfeng  Xie Xüiqiang
作者单位:SeismologicalBureauofJiangxiProvince,Nanchang330039,China
摘    要:The regional stress field and seismic dynamics along the border zone between Fujian, Guangdong and Jiangxi Provinces are studied based on the seismo-geological data, GPS measurement, and seismicity. The results show that: (1) the principal compressional stress of the stress field is oriented in NW-SE direction and the principal extensional stress is in NE-SW direction; (2) the WNW-ward compression and collision of the Philippine Sea Plate to the eastern coast of Taiwan Island are the most direct and most important dynamic source for preparation and occurrence of strong earthquakes in the Taiwan area and along the border zone between Fujian, Guangdong and Jiangxi Provinces.

关 键 词:动力学  GPS  测量方法  地震源  板块压力  江西  广东  福建

Regional Stress Field and Seismic Dynamics Along the Border Zone Between Fujian, Guangdong and Jiangxi Provinces
Zhang Fuping,Hu Cui''e,Wang Zhiguo,Huang Shuangfeng.Regional Stress Field and Seismic Dynamics Along the Border Zone Between Fujian, Guangdong and Jiangxi Provinces[J].Earthquake Research in China,2003,17(2):134-144.
Authors:Zhang Fuping  Hu Cui'e  Wang Zhiguo  Huang Shuangfeng
Institution:Seismological Bureau of Jiangxi Province, Nanchang 330039, China;Seismological Bureau of Jiangxi Province, Nanchang 330039, China;Seismological Bureau of Jiangxi Province, Nanchang 330039, China;Seismological Bureau of Jiangxi Province, Nanchang 330039, China;Seismological Bureau of Jiangxi Province, Nanchang 330039, China;Seismological Bureau of Jiangxi Province, Nanchang 330039, China
Abstract:The regional stress field and seismic dynamics along the border zone between Fujian, Guangdong and Jiangxi Provinces are studied based on the seismo-geological data,GPS measurement, and seismicity. The results show that: (1) the principal compressional stress of the stress field is oriented in NW-SE direction and the principal extensional stress is in NE-SW direction; (2) the WNW-ward compression and collision of the Philippine Sea Plate to the eastern coast of Taiwan Island are the most direct and most important dynamic source for preparation and occurrence of strong earthquakes in the Taiwan area and along the border zone between Fujian, Guangdong and Jiangxi Provinces.
Keywords:Border zone between Fujian  Guangdong and Jiangxi Provinces  Regional stress field  Dynamics  The GPS measurement  Seismicity
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