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- W2313403216 abstract "Slope failure phenomena which was caused by the CHI-CHI earthquake was investigated, and a following knowledge was obtained. The slope failures divided into two main types. The one is concurred with a large number of small-scale landslides which are moved at high speed, and the other is the enormous rock formation landslide. The fomer is mainly constituted sand and gravel layer of the plasticity or brittle hard rocks, and arise in strong motion area of above 250gal. The latter look at the pelitic rock regions. They are difficult to occure landslides caused by the earthquake in general. However, enormous landsildes arose by the CHI-CHI earthquake. It seems that is related to Buckling based on the defomation of the rock formation which is affected by fault activity and seating phemomena." @default.
- W2313403216 created "2016-06-24" @default.
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- W2313403216 date "2001-01-01" @default.
- W2313403216 modified "2023-09-25" @default.
- W2313403216 title "Some problems of the large-scale landslides caused by the Taiwan CHI-CHI earthquake from September 21st, 1999" @default.
- W2313403216 cites W2166095666 @default.
- W2313403216 doi "https://doi.org/10.3313/jls1964.37.4_33" @default.
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