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

DOI Web Site Web Site 被引用文献1件

収録刊行物

  • Lithos

    Lithos 119 (1-2), 10-19, 2010-09

    Elsevier BV

被引用文献 (1)*注記

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