FeNiCu sulfides in tectonite peridotites from the Maqsad district, Sumail ophiolite, southern Oman: Implications for the origin of the sulfide component in the oceanic upper mantle
- 1 September 1988
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 151 (1), 57-73
- https://doi.org/10.1016/0040-1951(88)90240-5
Abstract
No abstract availableKeywords
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