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.
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
关键词
融冻
泥石流
雪蚀洼地
昌马断裂带
Thawing debris flow
Nivation basin
Changma fault belt
