(Table 1) Chemistry of two samples of the red weathered layer at DSDP Hole 55-432A

2019-11-23T08:59:41Z (GMT) by Anne Marie Karpoff
One argument for the subaerial formation of Nintoku Seamount in the Emperor chain is the occurrence of a red claystone interlayered between two basalt flows in Hole 432A. Detailed study of this material, presented here, defines its nature and composition and strongly indicates its subaerial formation.

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