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Distribution Characteristics and Influencing Factors of Geological Hazards in Tibet
作者姓名:FAN  Jihui  WU  Caiyan  Cheng  Genwei
作者单位:[1]Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041, Sichuan, China; [2]Graduate University of Chinese Academy of Sciences, Beijing 100049, China
基金项目:国家重点基础研究发展计划(973计划);国家高技术与发展计划(863计划)
摘    要:0IntroductionTibet is located at26°50′-36°33′Nand78°25′-99°06′Ein the southwest of China,which isbounded by Sichuan,Yunnan,Qinghai Provincesand Xinjiang Uygur Autonomous Region and coun-tries suchas Nepal,India,Bhutan,Sikki mand My-anmar1].As main part of Qinghai-Tibet Plateau,Tibet has a special and complex geological condi-tion.Accordingtothe geotectonics,Tibet lies with-in the east of the huge Alps-Hi malayas mountainsystem.Because the Indian Plate continues divinginto no…

关 键 词:西藏  地质灾害  分布特征  影响因素  山崩
文章编号:1007-1202(2006)04-0806-07
收稿时间:2005-12-20

Distribution characteristics and influencing factors of geological hazards in Tibet
FAN Jihui WU Caiyan Cheng Genwei.Distribution Characteristics and Influencing Factors of Geological Hazards in Tibet[J].Wuhan University Journal of Natural Sciences,2006,11(4):806-812.
Authors:Fan Jihui  Wu Caiyan  Cheng Genwei
Institution:(1) Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, 610041 Chengdu, Sichuan, China;(2) Graduate University of Chinese Academy of Sciences, 100049 Beijing, China
Abstract:Tibet is one of the areas with most serious geological hazards in China, and the distribution of disasters has obvious local charac teristics. Tibet can be classified as three parts through zoning the danger degree, the mountain canyon high danger zone of east and southeast Tibet, the plateau mountain lake basin and valley middle danger zone of south Tibet, and the Plateau Mountain lake basin low danger zone of south Tibet. This paper takes the debris flow, collapse, landslide as the key points to analyze the distribution characteristics of geological hazards, and analyze the factors which influence the distribution of geological hazards, such as terrain landform, formation lithology, geologic structure pattern, precipitation, earthquake, human activity and so on. finally, as a conclusion., in whole Tibet, the geological hazards are more in southeast than in northwest, more in mountainous area which in the edge of plateau and river valley than in the interior of plateau and lake basin. And most hazards distribute in the regions where human activity is stronger than in other regions, for example towns or strips along the highway.
Keywords:Tibet  geological hazards  distribution characteristics  influencing factors
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