| 昌马断裂带触冻泥石流的基本特征 |
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| 引用本文： | 康来讯,王建荣.昌马断裂带触冻泥石流的基本特征[J].东北地震研究,1996,12(4):34-39. |
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| 作者姓名： | 康来讯 王建荣 |
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| 作者单位： | 国家地震局兰州地震研究所 |
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| 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，内部结构特征以及雪蚀洼地的特征及其形成机理等问题。
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| 关 键 词： | 融冻 泥石流 雪蚀洼地 昌马断裂带 |
BASIC CHARACTERISTICS OF THAWING DEBRIS FLOWS ALONG CHANGMA FAULT BELT |
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| Kang Laixun Wang Jianrong Wang Jinbao.BASIC CHARACTERISTICS OF THAWING DEBRIS FLOWS ALONG CHANGMA FAULT BELT[J].Seismological Research of Northeast China,1996,12(4):34-39. |
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| Authors: | Kang Laixun Wang Jianrong Wang Jinbao |
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| Abstract: | 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. |
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| Keywords: | Thawing debris flow Nivation basin Changma fault belt |
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