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《GEOLOGICAL SCIENCE AND TECHNOLOGY INFORMATION》 1997-03
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RELATIONSHIP OF LANDSLIP WITH TECTONIC MOVEMENT AND CLIMATIC CHANGE IN YANGTZE THREE GORGES

Li Changan (Faculty of Environmental Science and Geotechnique, China University of Geosciences,Wuhan,430074))  
Landslip is one of the most important geologic hazards in Three Gorges area.The formation of the landslip and its development are closely related to the stages of neotectonic movement in interrupted uplifting.The datings show that most landslips occurred in Quaternary warm and wet climate stages.Because the river terrace is the result of interrupting neotectonic uplift and its forming stages are bound up with the geologic climate cold warm changes,i.e.scarps form in cold stage,cumulates form in warm stage.Therefore,the forming process of terrace is the basis of landslip geomorphic process research in valley area.
【Fund】: 国家科委预研究项目
【CateGory Index】: P642.22
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