- Abstract:
-
Highly anomalous platinum-group element (PGE) concentrations in the podiform chromitites at the Cliff and Harold's Grave localities in the Shetland ophiolite complex have been well documented previously. The focus of this study is alluvial platinum-group minerals (PGM) located in small streams that drain from the PGE-rich chromitites. The placer PGM assemblage at Cliff is dominated by Pt-arsenides (64%) and Pd-antimonides (17%), with less irarsite–hollingworthite (11%) and minor Pd-sulfides, ...
Expand abstract - Publication status:
- Published
- Peer review status:
- Peer reviewed
- Version:
- Accepted Manuscript
- Files:
-
-
(pdf, 3.0MB)
-
- Publisher copy:
- 10.1180/minmag.2017.081.099
-
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- Publisher:
- Cambridge University Press Publisher's website
- Journal:
- Mineralogical Magazine Journal website
- Volume:
- 82
- Issue:
- Special Issue 3
- Pages:
- 491-514
- Publication date:
- 2018-04-16
- Acceptance date:
- 2017-12-17
- DOI:
- EISSN:
-
1471-8022
- ISSN:
-
0026-461X
- Pubs id:
-
pubs:935879
- URN:
-
uri:6e64a90d-37d4-40e4-8ee0-55d44d750548
- UUID:
-
uuid:6e64a90d-37d4-40e4-8ee0-55d44d750548
- Local pid:
- pubs:935879
- Copyright holder:
- Mineralogical Society of Great Britain and Ireland
- Copyright date:
- 2018
- Notes:
- © Mineralogical Society of Great Britain and Ireland 2018. This is the author accepted manuscript following peer review version of the article. The final version is available online from Cambridge University Press at: 10.1180/minmag.2017.081.099
Journal article
Placer platinum-group minerals in the Shetland ophiolite complex derived from anomalously enriched podiform chromitites
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