(Table 3) Geochemistry of clinopyroxene at DSDP Hole 82-556 peridotites

DOI

All iron (Fe*) is assumed to be Fe2+. All except sample 82-556-13-1,6-8 are exsolution blebs from much larger orthopyroxene.

Identifier
DOI https://doi.org/10.1594/PANGAEA.806237
Related Identifier https://doi.org/10.1594/PANGAEA.806240
Related Identifier https://doi.org/10.2973/dsdp.proc.82.129.1985
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.806237
Provenance
Creator Michael, Peter; Bonatti, Enrico ORCID logo
Publisher PANGAEA
Publication Year 1985
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 135 data points
Discipline Earth System Research
Spatial Coverage (-34.685 LON, 38.940 LAT); North Atlantic/RIDGE