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The Deformation of Active Tectonic Blocks on the Chinese Mainland and Its Relationship with Seismic Activity

机译:中国大陆活动构造块体的变形及其与地震活动的关系

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摘要

Based on the hypothesis of the active tectonic blocks on the Chinese continent and its adjacent regions (both the method of the DDA on a spherical surface and the GPS survey results observed from 1991 to 2001 are used), the movements and deformations of each active tectonic-block are calculated. The calculation results show that although the movements and deformations of active tectonic-blocks in the eastern region and in the western region of China are different, active tectonic blocks in the same active tectonic block region are coherent. Then, the relative velocities of the active tectonic-blocks' boundary zones are calculated, and the relationship between current crustal motion and strong seismic activities is discussed. Earthquakes (M_s ≥ 7.0) on the Chinese continent since 1988 all occurred on boundary zones of active tectonic blocks with high slipping speed.
机译:基于中国大陆及其邻近地区活动构造块的假说(采用球面DDA方法和1991年至2001年观测的GPS调查结果),每个活动构造的运动和变形-块被计算。计算结果表明,尽管中国东部和西部地区活动构造块的运动和变形是不同的,但同一活动构造块区域中的活动构造块是一致的。然后,计算了活动构造块边界带的相对速度,并讨论了当前地壳运动与强地震活动之间的关系。自1988年以来,中国大陆的地震(M_s≥7.0)都发生在滑动速度快的活跃构造块体的边界区域。

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