JOURNAL OF YANGTZE RIVER SCIENTIFIC RESEARCH INSTI ›› 2006, Vol. 23 ›› Issue (4): 17-22.
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LI Hui-Zhong, WANG Tuan-Le, DUAN Wei-Feng, SUN Li-Hua
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Abstract: The Jinpingzi Landslide, located in the downstream of the Wudongde Hydro -power Station about 900 m on Jinsha Rive r,was estimated 0.62 billion m3 by using remote sensing technology. The st ability, the movement trend and the possibility of the failure form are the key geological issues tha t have to be solved. On the basis of the geological mapping, drilling and shaft exploring, geophysical exploration and systematic TL dating and rock testing, a thorough investigation on the geological setting and the geological structure o f the landslide mass is represented. And the subzones are plotted out. The mec hanism of the sliding and the evolution of the Jingsha River are analyzed. The c onclusion is that the ancient landslide mass is located in the ancient river ch annel and ancient landslide is stable. This conclusion provides a strong basis t hat the hydro -power station could be constructed in the area and it also play a n important role for study the evolution of the Jinsha River. The achievements a nd the experience can be adopted for the other similar hydro -power projects that will be developed on Jinsha River.
LI Hui-Zhong, WANG Tuan-Le, DUAN Wei-Feng, SUN Li-Hua. Geological Study on Mechanism of Jinpingzi Landslide and Evolution of Landform of Jinsha River[J]. JOURNAL OF YANGTZE RIVER SCIENTIFIC RESEARCH INSTI, 2006, 23(4): 17-22.
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http://ckyyb.crsri.cn/EN/Y2006/V23/I4/17