The Origin and Mechanical Behavior of Colluvial Deposits at the LiShan area
碩士 === 國立交通大學 === 土木工程系所 === 96 === The Lishan colluvial deposits are composed of fractured slate and its weathered soils. The ground surface exhibits concave-convex relief which were formed by erosion. Thus, the terrain and geology indicate that landslide is easy to be triggered by rainfall or ea...
| Main Authors: | , |
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| Format: | Others |
| Language: | zh-TW |
| Published: |
2008
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| Online Access: | http://ndltd.ncl.edu.tw/handle/55417008961793726080 |