IMHE OpenIR  > 成都山地所知识仓储(2009年以前)
Alternative TitlePreliminary Inverstigation of Mud Flow in Area of the Loess Plateau
谭万沛; 张信宝; 王成华
Corresponding Author谭万沛
Source Publication人民黄河
Other Abstract 作者根据实地考察,概述了黄土高原区泥石流的分布、类型及活动特征。将全区分为七个活动性泥石流带,各带都有一定的东西向或南北向的差异性。在类型上泥流居多,但规模偏小,其活动性和规模主要决定于黄土崩塌、滑坡活动和降雨量的多少及强度。 
; Based on site inverstigation, the author describes distribution, type and charactrstics of mud fIow in area of loess plateau, which can be divided into 7 zones of activity of mud flow, each differential in East-West or South-North. As respect of the type, silt flow is prevailing but in relatively small scale. The activity and scale of silt flow is being controlled by collapse and slid of loess as well as rainfall. 
Keyword泥石流类型 黄土高原地区 黄土泥流 活动特征 粘性泥流 黄土崩塌 稀性泥石流 滑坡活动 活动性 降雨量
Document Type期刊论文
First Author Affilication中国科学院水利部成都山地灾害与环境研究所
Recommended Citation
GB/T 7714
谭万沛,张信宝,王成华. 黄土高原地区泥石流的初步考察[J]. 人民黄河,1987(3):22-26.
APA 谭万沛,张信宝,&王成华.(1987).黄土高原地区泥石流的初步考察.人民黄河(3),22-26.
MLA 谭万沛,et al."黄土高原地区泥石流的初步考察".人民黄河 .3(1987):22-26.
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