小江断裂带中段的北东向断裂与断块结构  

THE NE TRENDING FAULTS AND BLOCK STRUCTURE IN THE CENTRAL SECTION OF THE XIAOJIANG FAULT ZONE

作　　者：沈军[1] 汪一鹏[1] 宋方敏[1] 曹忠权[1] 申旭辉[1] 俞维贤[2] 侯学英[2] 李志祥[2] 

机构地区：[1]国家地震局地质研究所 [2]云南省地震局地震工程研究所

出　　处：《地震地质》1997年第3期203-210,共8页Seismology and Geology

摘　　要：小江断裂带中段东西支断裂间存在的ＮＥ向断裂是在第三纪ＮＥ向断裂的基础上，于第四纪中晚期开始新的活动，并具有左旋走滑运动的特征，有些在全新世仍有活动。它们的活动从属于小江断裂带的整体左旋走滑运动，其运动幅度和速率比近ＳＮ向小江东西支断裂小得多，但是由于它们的运动，使主断裂产生弯曲或阶区，形成有利于应力和应变集中的障碍。夹于东西支断裂之间的断块被ＮＥ向断裂切割为多个次级菱形和梭形断块，这些断块之间的相对运动对断裂分段和地震孕育过程具有不可忽视的影响。The middle section of the Xiaojiang fault zone located in Yunnan Province is branched into east and west two faults. Between these faults there are many NE trending smaller faults and blocks cuted by nearly SN and EW trending faults. They make up the network shape structure with rectangular geometry of the middle section of the Xiaojiang fault zone. These NE trending faults inherited those of Tertiay and were innovated in Quartary with left lateral slip. Some of them have been active till Holocene. Their activities belong to the integrated left lateral slip motion of the Xiaojiang fault zone with much smaller magnitude and rate comparing with the main faults. Because of their motion the main faults have bending or step areas which are barries for stress and strain concentration. The blocks between the east and west main faults are cut by the NE trending faults into many secondary blocks of diamond and shuttle shape. Relative movements occur between these blocks which have important effect on the segmentation of faults as well as earthquake occurrence.

关 键 词：小江断裂 断块构造 断层活动 地震地质 

分 类 号：P542.3[天文地球—构造地质学]