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    Volume 28 Issue 3
    May  2003
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    Article Contents
    ZHOU Cheng-hu, PEI Tao, LI Quan-lin, CHEN Jin-biao, WANG Zhuo-sen, 2003. Research on Spatial Pattern and Temporal-Spatial Migration Model of Strong Earthquakes in China and Its Adjacent Areas. Earth Science, 28(3): 306-314.
    Citation: ZHOU Cheng-hu, PEI Tao, LI Quan-lin, CHEN Jin-biao, WANG Zhuo-sen, 2003. Research on Spatial Pattern and Temporal-Spatial Migration Model of Strong Earthquakes in China and Its Adjacent Areas. Earth Science, 28(3): 306-314.

    Research on Spatial Pattern and Temporal-Spatial Migration Model of Strong Earthquakes in China and Its Adjacent Areas

    • Received Date: 2002-12-25
    • Publish Date: 2003-05-25
    • The development of the seismic database of China and its adjacent areas is introduced in the first part of this paper. Based on the combination of the difference between western and eastern parts of China on plate tectonics, stress state and structure of crust-mantle, the authors analyze the spatial pattern of strong earthquakes from aspects of the whole dataset, historical seismic records, instrumental records and hypocenter depth. It is found that before 1900 DC, North China presented the great trapeziform pattern. After 1900 DC, the west part of China was characterized by the huge sector, with the deepest regions of foci located in the two vertices of the huge sector, namely Xingdukushi-Pamier region and the area along the border of India and Burma. Then, the linear and regional migrating modes are summarized according to the spatial pattern of strong earthquakes in China. Detailedly, the linear migration can be subdivided into two modes, straight jumping and pendulum. The mechanisms of all types of migrating modes are briefly discussed based on the models of fault fracture, spring-block, structural difference between crust and mantle and their relative movement as well.

       

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