LARGE-SCALE STRIKE SLIP FAULT: THE MAJOR STRUCTURE OF INTRACONTINENTAL DEFORMATION AFTER COLLISION

查看全文 作　　者：[1]钟大赉;P. [2]TAPPONNIER;[1]吴海威;[1]张连生;[1]嵇少丞;[1]钟嘉猷;[1]刘小汉;U. [2]SCHAERER;R. [2]LACASSIU;P. [2]LELOUP 机构地区：[1]Institute of Geology, Academia Sinica, Beijing 100011, PRC;[2]Institule of Geophysics.C.N.R.S.France 出　　处：《Chinese Science Bulletin》索引1990年第35卷第4期,共6页 基　　金：Project supported by the National Natural Science Foundation of China and C. N. R. S., France. 摘　　要：Intracontinental deformation is one of the most interesting problems in tectonics. But so far little attention has been paid to rock deformation, metamorphism and magmatism related with large-scale displacement and rotation of these blocks. In this note, we take the Ailaoshan-Red River fault (ARF)zone in western Yunnan as an example and discuss the kinematics and dynamics of the fault With its neighbouring blocks in the Tertiary. 关 键 词：intracontinental DEFORMATION LARGE-SCALE STRIKE SLIP Ailaoshan-Red River fault.