Platinum-group elements in rocks from the voikar-syninsky ophiolite complex, Polar Urals, U.S.S.R.
Mineralium Deposita
By: N.J. Page, P. J. Aruscavage, and J. Haffty
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Abstract
Analyses of platinum-group elements (PGE) in rocks collected from the Voikar-Syninsky ophiolite in the Polar Urals suggest that the distribution and geochemistry of PGE in this Paleozoic ophiolite are similar to those in Mesozoic ophiolites from elsewhere. Chondrite-normalized PGE patterns for chromitite, the tectonite unit, and ultramafic and mafic cumulate unit have negative slopes. These results are similar to those found for chromitites from other ophiolites; stratiform chromities show positive slopes. If the magmas that form both types of chromitite originate from similar mantle source material with respect to PGE content, the processes involved must be quite different. However, the distinct chondrite-normalized PGE patterns may reflect differing source materials. ?? 1983 Springer-Verlag.
Suggested Citation
Page, N., Aruscavage, P.J., and Haffty, J., 1983, Platinum-group elements in rocks from the voikar-syninsky ophiolite complex, Polar Urals, U.S.S.R.: Mineralium Deposita, v. 18, no. 3, p. 443-455, https://doi.org/10.1007/BF00204489.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Platinum-group elements in rocks from the voikar-syninsky ophiolite complex, Polar Urals, U.S.S.R. |
| Series title | Mineralium Deposita |
| DOI | 10.1007/BF00204489 |
| Volume | 18 |
| Issue | 3 |
| Year Published | 1983 |
| Language | English |
| Publisher location | Springer-Verlag |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Mineralium Deposita |
| First page | 443 |
| Last page | 455 |