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Publications by [Luo G.]
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<p>Tangjiashan landslide is a typical high-speed landslide hosted on consequent bedding rock. The landslide was induced by Wenchuan earthquake at a medium-steep hill slope. The occurrence of Tangjiashan landslide was basically controlled by the tectonic structure, ...
Filed under: Soil Mechanics - Numerical MethodsReference: Journal of Rock Mechanics and Geotechnical Engineering. 2012, 4 (2): 149–159