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

DOI

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.

Supplement to: Karpoff, Anne Marie (1980): The claystone layer between two basalt flows in Hole 432A: An argument for the emergence of Nintoku Seamount. In: Jackson, ED; Koisumi, I; et al., (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 55, 707-711

Identifier
DOI https://doi.org/10.1594/PANGAEA.823433
Related Identifier https://doi.org/10.2973/dsdp.proc.55.132.1980
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.823433
Provenance
Creator Karpoff, Anne Marie
Publisher PANGAEA
Publication Year 1980
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Dataset; Dataset
Format text/tab-separated-values
Size 56 data points
Discipline Earth System Research
Spatial Coverage (170.379 LON, 41.334 LAT); North Pacific/TERRACE