A RELATIONSHIP BETWEEN RIVERINE LANDSLIDE AND HYDRODYNAMISM IN UPPER COURCE OF YANGTZE RIVER(THE SECTION FROM CHONGQING TO PEISHI)

doi:10.6046/gtzyyg.1990.01.08

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Abstract

In this paper analyses of stream pattern and fluvial land form and hydro logical regime suggest that a stability of shore Yangtze's in addition to lithlogical character and structural condition, depends particularly on a roe fluvial land form and hydrodynamic process in formation of landslides along the upper course. For example a remobilization of landslide at Jipaz Yunyang County Sichuan Province on July 1982 shows that no considering geologic process of river has been landslide controlled is inopportunely.

Keywords Landuse Vector to Raster Accuracy Loss

Issue Date: 02 August 2011

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	ZhAO Lei
	MENG Shu-Yang
	ZHANG Hua-zhong
	LIAN Hong-tao
	SUI Qi-fa

Cite this article:

ZhAO Lei,MENG Shu-Yang,ZHANG Hua-zhong, et al. A RELATIONSHIP BETWEEN RIVERINE LANDSLIDE AND HYDRODYNAMISM IN UPPER COURCE OF YANGTZE RIVER(THE SECTION FROM CHONGQING TO PEISHI)[J]. REMOTE SENSING FOR LAND & RESOURCES, 1990, 2(1): 47-52.

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https://www.gtzyyg.com/EN/10.6046/gtzyyg.1990.01.08 OR https://www.gtzyyg.com/EN/Y1990/V2/I1/47

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