Decreased slip rate on the Kunlun fault zone since ~100 ka, constrained by offset alluvial fan and cosmogenic nuclide dating

Junjie Ren1, Xiwei Xu1, Feipeng Huang2, Yanwu Lyu1, Oubo Liang1 and Junxiang Zhao1, (1)Institute of Crustal Dynamics, China Earthquake Administration, Beijing, China, (2)China Earthquake Administration, Beijing, China
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