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    Volume 33 Issue 2
    Mar.  2008
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    YE Xing-shu, WANG Wei-feng, 2008. Plate Subduction Contrains on the Formation of Jiyang Depression. Earth Science, 33(2): 235-242.
    Citation: YE Xing-shu, WANG Wei-feng, 2008. Plate Subduction Contrains on the Formation of Jiyang Depression. Earth Science, 33(2): 235-242.

    Plate Subduction Contrains on the Formation of Jiyang Depression

    • Received Date: 2007-05-12
    • Publish Date: 2008-03-25
    • In order to research the influence of mantle plume tectonics and plate subduction on the Jiyang depression, the geological characteristics of Jiyang depression and the results of the seismic source of earthquake and plate subduction are analyzed, based on the preview studies of the mantle plume.The result shows that the sedimentary stratum, the activities of magma, geological extension, the grads of terrestrial, and the reservoir sand are distributed regularly from south to north in Jiyang depression.The process of plate subducting into mantle formed the downwelling of mantle convection, the depth of 660 km (or 670 km) of the mantle is the depth of the upwelling which was adjusted by the matter of mantle after plate subducting into mantle.The downthrust angle of the subduction of western Pacific plate decreases from south to north, and the time of subducted plate reaching the discontinutity surface of earthquake increases from south to north, which resulted in the mantle plume transfer from south to north and regular distribution of the geology, geophysical characteristics from south to north in Jiyang depression.

       

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