云南东川小江泥石流
文献类型：专著章节文集论文
| 语种 | 中文 |
| 作者 | 陈循谦1; 杨文科1; 牛宪锟1; 康志成2 ; 章书成2; 陈景武2
|
| 发表日期 | 1981-12 |
| 页码 | 13-19 |
| 出版者 | 科学技术出版社重庆分社 |
| 出版地 | 重庆 |
| 关键词 | 暴雨泥石流 小江流域 东川 云南 |
| 交替题名 | Debris Flows Along the Xiaojiang River, DongChuan, Yunnan |
| 英文摘要 | The Xizang area has undergone strong uplift since Neogene. With unique natural conditions favourable to the occurrence and development of debris flows, it is one of the regions where debris flows are most developing and active in China. In Xizhang there are two kinds of water sourcesforming debris, i.e, rainwater and meltwater. The former causes rainfall debris flows, and the latter triggers glacial debris flows. The development and distribution of debris flows in Xizang vary with landforms and climate. In the interior of Xizang, debris flows are not developing for the weather is parching and cold. On the other hand, both types of debris flows are widdy distributed and strong in acitivity in mountainous region of Southeast and South Xizang with a humid and rainy climate,and much meltwater in summer. That is the chief region of debris flows in Xizang. The distribution of debris flows has a vertical zonation. Glacial debris flows orginate in the alpine ice and snow belt; rainfall debris flows in the forest or sparse brush belt. The activity of debris flows in Xizang with a long history is characterzied by rhythm, which is related to the rhythm of the climate and sesmic activity. |
| 源URL | [http://ir.imde.ac.cn/handle/131551/26978]  |
| 专题 | 成都山地灾害与环境研究所_成都山地所知识仓储（2009年以前） |
| 作者单位 | 1.云南省东川市小江整治办公室; 2.中国科学院成都地理研究所 |
| 推荐引用方式 GB/T 7714 | 陈循谦,杨文科,牛宪锟,等. 云南东川小江泥石流. 重庆:科学技术出版社重庆分社,1981:13-19. |
入库方式： OAI收割
来源：成都山地灾害与环境研究所
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