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Ojén Iherzolite massif, Ojén, Málaga, Andalusia, Spain
Platinum-group minerals (PGM) occur as discrete inclusions in the chromite and in the associated silicates. Textural considerations suggest that the PGE chalcogenides with S and As were formed in the high-temperature magmatic stages, as part of the chromite precipitation event (primary PGM), in contrast with the native PGE, which originated during the low-temperature serpentinization of the ultramafic host of the chromitites (secondary PGM) (Torres-Ruiz, et al., 1996).
Refs.:
- Garuti, G., Gazzotti, M., and Torres-Ruiz, J. (1995) Iridium, rhodium, and platinum sulfides in chromitites from the ultramafic massifs of Finero, Italy, and Ojen, Spain. Canadian Mineralogist: 33: 509-520.
- Torres-Ruiz, J., Garuti, G., Gazzotti, M., Gervilla, F., and Hach-Alí, P.F. (1996) Platinum-group minerals in chromitites from the Ojen Iherzolite massif (Serrania de Ronda), Betic Cordillera, southern Spain. Mineralogy and Petrology: 56: 25-50.
Mineral List
Mineral list contains entries from the region specified including sub-localities37 entries listed. 29 valid minerals. 1 type locality (valid mineral).
Localities in this Region
Spain
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New Locality Added: Pougamaro River placers, Pala, Mayo-Kebbi Ouest Region, ChadFrom David Von Bargen, 21st May 2013 14:05:47
















