昌马断裂带触冻泥石流的基本特征  

BASIC CHARACTERISTICS OF THAWING DEBRIS FLOWS ALONG CHANGMA FAULT BELT

作　　者：康来迅[1] 王建荣[1] 王进保 

机构地区：[1]国家地震局兰州地震研究所

出　　处：《东北地震研究》1996年第4期34-39,共6页Seismological Research of Northeast China

基　　金：地震科学联合基金

摘　　要：根据详细的野外地质调查和地质探槽资料，本文讨论了昌马断裂带融冻泥石流的形态特征。Based on the detailed data of field geological investigation and geological trenching,the characteristics of formation and internal structure of thawing debris flowina,the features of nivation basin and their forming mechanism along changma fault belt and discussed in this paper.

关 键 词：融冻 泥石流 雪蚀洼地 昌马断裂带 

分 类 号：P642.23[天文地球—工程地质学]