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通过对1605年琼州7.5级大地震震中区及邻近地区大地电磁探测,发现震中区地壳深部存在一低阻体.该低阻体自约13 km以下一直延伸到上地幔,推测其为正在上升的地幔柱,并由此认为地幔柱的存在及其热物质的上涌,使上部地壳产生断裂和粘滑活动,是产生琼州7.5级大地震的重要原因.这次大地震后断裂活动表现为以蠕滑为主.推测未来再发生同等强度大地震的危险性将大大降低.  相似文献
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From the magnetotelluric detection in the epicentral region and the adjacent areas of the 1605 M7.5 Qiongzhou earthquake, we have discovered there is a low resistive body in the deep crust of the epicentral region. The low resistive body extends straightly from the depth of about 13 km to the upper mantle, which is supposed as an up-rising mantle pole. We therefore consider it is just the existing mantle pole and its upwelling thermal material that result in the faulting and stick-slipping activities of the upper crust, which is an important factor for the M7.5 Qiongzhou great earthquake occurrence. The postseismic faulting activity is characterized by creep, which shows that the risk is greatly decreased for the occurrence of a great earthquake with similar intensity in the future.  相似文献
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