State shift in Deccan volcanism at the Cretaceous-Paleogene boundary, possibly induced by impact
Abstract
Bolide impact and flood volcanism compete as leading candidates for the cause of terminal-Cretaceous mass extinctions. High-precision 40Ar/39Ar data indicate that these two mechanisms may be genetically related, and neither can be considered in isolation. The existing Deccan Traps magmatic system underwent a state shift approximately coincident with the Chicxulub impact and the terminal-Cretaceous mass extinctions, after which ~70% of the Traps'...
Paper Details
Title
State shift in Deccan volcanism at the Cretaceous-Paleogene boundary, possibly induced by impact
Published Date
Oct 1, 2015
Journal
Volume
350
Issue
6256
Pages
76 - 78
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