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Regional Stress Field and Seismic Dynamics Along the Border Zone Between Fujian, Guangdong and Jiangxi Provinces

机译:闽粤赣边沿区域的区域应力场与地震动力学

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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.
机译:基于地震地质数据,GPS测量和地震活动性,研究了福建,广东和江西两省交界处的区域应力场和地震动力学。结果表明:(1)应力场的主压应力为NW-SE方向,主拉伸应力为NE-SW方向; (2)菲律宾海床向台湾岛东海岸的西北偏西压缩和碰撞,是台湾地区以及福建两岸边界地区发生强震的最直接,最重要的动力源,广东省和江西省。

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