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

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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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2018-01-30
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