Petrology and geochemistry of basalt at DSDP Hole 66-487

DOI

Major oxide and trace element determinations of the composition basalts from the bottom of Hole 487, together with microprobe analyses of their minerals (olivine, magnesiochromite, salite, and plagioclase), prove that they are depleted oceanic tholeiites.

Supplement to: Joron, Jean Louis; Bougault, Henri; Maury, R C; Stephan, J F (1982): Basalt from the Cocos Plate, Site 487, Leg 66: Petrology and geochemistry. In: Watkins, JS; Casey Moore, J; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 66, 731-734

Identifier
DOI https://doi.org/10.1594/PANGAEA.817825
Related Identifier IsSupplementTo https://doi.org/10.2973/dsdp.proc.66.136.1982
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.817825
Provenance
Creator Joron, Jean Louis; Bougault, Henri; Maury, R C; Stephan, J F
Publisher PANGAEA
Publication Year 1982
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Publication Series of Datasets; Collection
Format application/zip
Size 3 datasets
Discipline Earth System Research
Spatial Coverage (-99.175 LON, 15.853 LAT); North Pacific/TRENCH