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川西高原主要地质灾害特征及其影响因素浅析
引用本文:段丽萍,郑万模,李明辉,邓国仕,杨桂花.川西高原主要地质灾害特征及其影响因素浅析[J].沉积与特提斯地质,2005,25(4):95-98.
作者姓名:段丽萍  郑万模  李明辉  邓国仕  杨桂花
作者单位:成都地质矿产研究所,四川,成都,610082
摘    要:川西高原位于青藏高原东缘,是崩塌、滑坡和泥石流等突发性地质灾害的群发地,具有分布基本沿活动构造带走向、发生时间较集中、人类活动诱发的地质灾害数量增多和地质灾害链后果严重等特点,主要受地质构造、现今构造运动、地形地貌、降雨及人类不科学的社会、经济和工程活动等多种因素影响。

关 键 词:地质灾害  川西高原
文章编号:1009-3850(2005)04-0095-04
收稿时间:2005-04-08
修稿时间:2005-04-08

Geologic hazards on the western Sichuan plateau and their controls
DUAN Li-ping,ZHENG Wan-mo,LI Ming-hui,DENG Guo-shi,YANG Gui-hua.Geologic hazards on the western Sichuan plateau and their controls[J].Sedimentary Geology and Tethyan Geology,2005,25(4):95-98.
Authors:DUAN Li-ping  ZHENG Wan-mo  LI Ming-hui  DENG Guo-shi  YANG Gui-hua
Institution:Chengdu Institute off Geology and Mineral Resources, Chengdu 610082, Sichuan , China
Abstract:The western Sichuan plateau lies on the eastern margin of the Qinghai-Xizang Plateau,where(abundant) violent geologic hazards such as collapse,landslide and debris flows frequently occur because of(complx)(geological) tectonics,active endokinetic/exokinetic processes and severe tectonization.These geologic hazards are generally aligned along active structural zones, and mostly controlled by geological structures,present-day(tectonic) movements,topography and geomorphology,rainfalls and human's activities in the study area.
Keywords:geologic hazard  western Sichuan plateau
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