Analysis of buckling failure process for the Xiaguiwa landslide in southeastern Tibetan Plateau
QUARTERLY JOURNAL OF ENGINEERING GEOLOGY AND HYDROGEOLOGY(2022)
摘要
Detailed field investigations at the Xiaguiwa landslide in the southeastern Tibetan Plateau (China) demonstrated how deep-seated buckling deformation can develop in a rapid slope failure. The results suggest that there exist three distinct phases during the buckling failure process: the moderately deformed phase, the heavily deformed phase and the failure phase. The Xiaguiwa landslide finally blocked the Jinsha River, formed a dammed lake and produced lacustrine deposits; these results represent common post-failure features associated with a rapid large landslide in the high-relief region in the Tibetan Plateau.
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