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Dynamics of the 2008 earthquake-triggered Wenjiagou Creek rock avalanche, Qingping, Sichuan, China
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文摘

We investigate dynamics and transport mechanism of Wenjiagou Creek rock avalanche.

Dynamic course is divided into three segments: the failing, the falling and the flow.

Structure of the deposit was determined by grain-size distribution analysis.

Ring-shear tests were conducted to simulate the shear between grains within debris.

Shear resistance between grains decreases due to pervasive fragmentation.

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