Based on the geological and geophysical data,this paper establishes a stereogeologic model of the Changma basin. The change of stress field and theearthquake mechanism be-fore and after the Changma Ms7.6 earthquake in 1932 are studied by 3-D finite element-method. The results show that: 1.The difference between the focal fault strike and that inferred by the principal com-pression stress is 65°,this probably is due to the block rotation which results from the force moment produced by the rotated principal compression stress in shallow crust and the NE directional principal compression stress in depth. The hinge point is the focal re-gion.The block rotation results in the differences between the mechanical and geometrical natures of earthquake fault and focal tault. 2.The Changma earthquake is due to the cooperative interaction of closing joint and block rotation. 3.The regional stress field discords with local stress field and the appearance of stress relaxation unit is probably relative tothe earthquake preparation and occurrence. 4.Nonuniformity of fault activity is positive correlative with the inhomogeneous dis-tribution of plane maximum shearing stress.The fracture zones are characterized by rela-tive levorotation, shove and compression,but the distribution of strike slip is inhomoge-neous.
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李步云.昌马地震应力场及发震机制研究[J].地震工程学报,1994,16(3):14-23. Li Buyun. RESEARCH ON STRESS FIELD AND CAUSATIVE MECHANISM OF THE CHANGMA EARTHQUAKE, GANSU PROVINCE[J]. China Earthquake Engineering Journal,1994,16(3):14-23.