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

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Title
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
Authors
Keywords
-
Journal
LITHOS
Volume 119, Issue 1-2, Pages 10-19
Publisher
Elsevier BV
Online
2010-06-14
DOI
10.1016/j.lithos.2010.06.001

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