PGE and Chalcophile element concentrations in peridotitic sulfides from the St. Elena ophiolite, Costa Rica
Abstract:
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. Accessed 2024-04-25.
DOI Creation Date:
2016-05-11
Related
Publication(s):
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.
License:
Creative Commons Attribution-NonCommercial-Share Alike 3.0 United States [CC-BY-NC-SA-3.0]
Funding source(s):
National Science Foundation:
1347890Keyword(s):
Coverage Scope: Regional (Continents, Oceans)
Geographic Location: St. Elena, Costa Rica
User Contributed Keyword(s):
ophiolite, peridotite, sulfide, platinum group elements
Bounding Coordinates:
North: 11.095 South: 10.95444 East: -85.78 West: -86.10611
Data Available On:
2016-09-01