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Geomorphologic Studies on Landslide Developmnt In Boundary Area of East Qinghal-xizang Plateau(Taking Douyapeng landstide as a example,wanxian)
Chen Hongkei, Tang Hongmei, Wang Jianpin
1994, 13(1):
86-93.
Larger landslides,developing in the boundary area of east Qinghai-Xizang plateau,have a direet bearing on zonal geomorphologie stress field in some extent.This paper discusses the relationships between landslides and geomorpholgy based on field investigations and analyse in home taking Douyapeng landstode as a example.It is important to providc the spinning uphcaval model of Qingkaj-Xizang p ateau,whieh ean explain reasonlythe formation and distribution of zonal stress field of the boundary area of east or all Qinghai-Xizang plateau.Generally,main moving direetions of many large landslides are eonsistent with either main oriention or shearbelt of the stress field Douyapeng landslide belongs to a larger landslide with two slide planes(the up one andthe down one).The up one is made gy mankind engineering aetions,and the down one is eontrolled by the zon-al stress ficld. valuablly,NE29°30′, chieffy moving direction of the landshde,is consistent with basis of drillresrlts,it is sure that the landsliole, develping late Quaternary,is consist of loose soils or earth and has clearcreep strain. we study the interest inthe paper for mankind actions to trigger the landslids too,and eoneludethat slope excavation、slope load and rich underyrourd water are the basic features for urban geomorpholyicproeess to cvaluate.The administration measures must be therefore syntheiical ones with engineering manner、governing water and adminestering way,whieh also be the general prineiples for Mt.city unstable slope to beruled.?
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