It is often observed that there are separated graben structures in the reactivated cratons where rifting occurred durig different poriods of their evolution. Some of these graberls behave as present-day active seismic zones,such as the Linfen graben, Shanxi,China; the Xingtai graben, Hebei, China; and the New Madrid graben, the United states. Increasing data have demonstrated that the causes of earthquakes in these areas are in-volved with many geological and geophysical conditions besides the active fauting.As a typical case,studies on the Luifen graben show that the seismogenic process is associated with the foliowing factors:(1)The metamorphic rocks with greater strength around the graben,in which stress is built up under the action of the regional tectonic stress field.(2)The medium of the seismogenic layer with lower strength at the depth range of 5 15 km within the graben,which ruptures during the seismic source process to release energy and radiate seismic waves. (3)The abnomal layer with low velocity or low resistance beneath the seismogenic layer,which has the ductle adjusting function to the seismic source process.(4)The fault zones along the both sides of the graben ,which are character-ized by mylonitization and have controlling effects on the process of earthquake brewing.The combination of these elements offers seismogenic models which can explain the causes of some seismic zones in the continental ar-eas associated with reactivated cratons and refting grabens.Numerical modeling has been used to test the pro-posed models.
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高祥林.大陆活化克拉通与裂谷地堑地区的地震构造模型[J].地震工程学报,1994,16(3):95-101. Gao Xianglin. SEISMOTECTONIC MODELS FOR THE CONTINENTAL AREAS ASSOCIATED WITH REACTIVATED CRATONS AND RIFTING GRABENS[J]. China Earthquake Engineering Journal,1994,16(3):95-101.