泰国北部梅江断裂的几何结构及其新活动的地貌标志  

THE GEOMETRIC STRUCTURE AND THE GEOMORPHIC SIGHS OF NEO-ACTIVITY IN THE MAE CHAN FAULT IN NORTH THAILAND

作　　者：韩新民[1] 毛玉平[1] 张建国[1] 杨继武[1] 

机构地区：[1]云南省地震局,昆明650041

出　　处：《地震研究》2000年第1期67-71,共5页Journal of Seismological Research

摘　　要：根据对泰国北部梅江断裂实地考察结果的分析 ,认为该断裂在几何结构上为一条由多条断层组成的复杂的断裂带 ,且反映断裂第四纪以来新活动的地貌标志突出。Based on analysis of the results on the spot investigation,It is thought that the Mae Chan fault is a complicated fault zone composed of many faults.The geomorphic signs reflecting the neo-activity in the fault since Quaternary Period are very deveolped along the fanlt.

关 键 词：梅江断裂 几何结构 地貌标志 断层 泰国 

分 类 号：P542.3[天文地球—构造地质学]