The Guadalupian–Lopingian boundary mudstones at Chaotian (SW China) are clastic rocks rather than acidic tuffs: Implication for a temporal coincidence between the end-Guadalupian mass extinction and the Emeishan volcanism

Bin He(Chinese Academy of Sciences), Junpeng Guan(Jiangsu Provincial Institute of Geological Survey), Yi‐Gang Xu(Chinese Academy of Sciences), Yuting Zhong(Chengdu Medical College)
Lithos
June 14, 2010
10.1016/j.lithos.2010.06.001
Cited by 177

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