PRELIMINARY STUDY OF THE RELATION BETWEEN THE DISTRIBUTION OF DISPLACEMENT AND THE RUPTURED STATE OF THE SEISMOGENIC FAULT

[1] 邓起东,1984.断层性状、盆地类型及形成机制.地震科学研究,3: 56—64.

[2] Deng Qidong, Wu Daning, Zhang Peizhen, Chen Shefa, 1986. Structural and deformational character of strike—slip fault zone. Pure and Applied Geophsics, 124, 1/2, 203—223.

[3] 邹定元,1984.我国走滑型断层地震地裂缝水平位移分布的考察与研究.地震科学研究,2: 1—10.

[4] 吴章明,邓起东,1989.西藏崩错八级地震地表破裂的形变特征及破裂机制.地震地质,11, 1, 15—25.

[5] Tchalenko J. S., Berberian M., 1975. Dasht—e Bayaz fault, Iran: earthquake and earlier related structure in bed rock. Geol. Soc. Am. Bull., 86, 703—709.

[6] Deng Qidong, Zhang Peizhen, 1984. Research on the geometry of shear fractures zones,J. Geophys. Res, 89, B7, 5699—5710.

[7] Chinnery M. A., Petrak J. A., 1968. The dislocation fault model with a variable discontinuity.Tectonophysics, 46, 513—529.

[8] Hildebrand—Mittlefehldt N., 1979. Deformation near a fault termination. Part I: A fault in a clay experiment. Tectonophysics, 57, 131—150.

[9] 余洋,梅世蓉,庄灿涛,1986. 模拟震源动力学破裂过程的数值方法研究.地球物理学报,29, 567—577.