走滑断裂带中挤压阶区内部剪切构造初探  

PRELIMINARY STUDY OF THE INNER SHEAR STRUCTURES IN THE COMPRESSIONAL STEPOVER OF STRIKE SLIP FAULT ZONES

作　　者：宋方敏[1] 俞维贤 

机构地区：[1]中国地震局地质研究所 [2]云南省地震工程研究院

出　　处：《地震地质》1998年第4期343-348,共6页Seismology and Geology

摘　　要：野外地质调查和航片立体镜下解译发现，小江断裂带北段蒙姑和东支大营盘两个挤压阶区内部发育有剪切构造，它们在地表主要表现为断裂槽地、断层陡坎、地裂缝等。挤压阶区内部剪切构造和拉张阶区内部剪切构造一样，是阶区形成后，随着走滑断裂的进一步活动而形成的新生性构造。Field investigation and airphoto interpretation have revealed that shear structures were developed in two compressional stepovers at Menggu on the northern segment of Xiaojiang fault zone and Dayingpan on the eastern branch of the fault zone. The shear structures appear on the earth surface mainly as fault troughes, fault scarps, surface fissures, beaded ponds and depressions. The inner shear structures in Menggu stepover extend about 5km, while those in Dayingpan stepover for about 3km. The results of high pressure and high temperature triaxial compression experiment, finite element analysis of fault dynamics of en echelon fault system and the deformation modeling of en echelon faults, have also indicated that the inner shear structures in compressional stepover are the same as those in the extensional stepover. They are newest active structures that are formed in stepover due to the action of local shear stress during the long term activity of the strike slip fault zone. The innner shear structures are intermittently outcropped on the earth surface. However, they are geomorphically less distinct than the shear faults controlling the boundary of the stepover. The inner shear structures in stepover display obvious recent activity. Historical and modern earthquakes often produced surface fractures along these structures. The surface fractures produced by the Dongchuan M 73/4 earthquake of 1733 were distributed just along the inner shear structures of Menggu and Dayingpan stepovers.

关 键 词：走滑断层 剪切构造 挤压阶区 走滑断裂带 

分 类 号：P542.3[天文地球—构造地质学] P542.2[天文地球—地质学]