PGE and Chalcophile element concentrations in peridotitic sulfides from the St. Elena ophiolite, Costa Rica
This dataset presents in situ (LA-ICPMS; down to a 10 micron beam size) major, minor, PGEs and chalcophile elements on sulfides from five partially serpentinized peridotites from the St. Elena ophiolite, Costa Rica. PGE-Re concentrations in sulfides (dominant petlandites) are highly variable, ranging from 1 – 100,000 times that of primitive mantle (PM). PM-normalized PGE-Re patterns in the sulfides are dominated by strong Pt depletions relative to Os, Ir, Ru and Pd. Pb concentrations average around 2.7 ppm.
How to cite this dataset:
Bizimis, M., Holm, J. A., 2016. PGE and Chalcophile element concentrations in peridotitic sulfides from the St. Elena ophiolite, Costa Rica, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.1594/IEDA/100589.
DOI Creation Date:
Holm, J., M. Bizimis, E. Schwarzenbach, D. Foustoukos, C. Frisby, A. Brandon, and E. Gazel (2015), Platinum group and chalcophile element systematics of serpentinized peridotites from the St. Elena ophiolite in Costa Rica, in AGU Fall Meeting, pp. V53B-3136, San Francisco, URL: https://agu.confex.com/agu/fm15/meetingapp.cgi/Paper/73156.
Creative Commons Attribution-NonCommercial-Share Alike 3.0 United States [CC-BY-NC-SA-3.0]
Coverage Scope: Regional (Continents, Oceans)
Geographic Location: St. Elena, Costa Rica
User Contributed Keyword(s):
ophiolite, peridotite, sulfide, platinum group elements
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