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- W2362061722 abstract "The geological process of landslide in the Three Gorges Reservoir area of Yangtze River is affected by the factors of three levels, i.e. deep structure of lithosphere, surface geological structure and new morphostructure. The formation and distribution of landslide geological hazard is controlled by the composite condition of structure, lithology and landform. The centralized distribution part of the massive landslide body was controlled by circular structure of northeast direction in the Three Gorges Reservoir area. The large rockfalls in the area mainly happened in the distribution zone of the thick limestone glint; The large landslide was mainly occurred in the belt of the slope bank formed by weak stratum on the edge of Jura type syncline, and might be summed up the four types of the lithologic structure. On the basis of information mentioned above, the division and forecast for the area of large easily occurred landslide body have been carried out on the both banks in the Three Gorges Reservoir area." @default.
- W2362061722 created "2016-06-24" @default.
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- W2362061722 date "2000-01-01" @default.
- W2362061722 modified "2023-09-25" @default.
- W2362061722 title "Study on the formation and distribution of landslide geological hazard in the Three Gorges Reservoir area" @default.
- W2362061722 hasPublicationYear "2000" @default.
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