Orthopyroxenite hosted chromitite veins anomalously enriched in platinum-group minerals from the Havana-Matanzas Ophiolite, Cuba
The Havana–Matanzas Ophiolite contains one of the few examples of ophiolitic platinum group minerals (PGM)-rich chromitites associated with orthopyroxenites in the mantle section of ophiolitic complexes. The chromitites occur as veins hosted by orthopyroxenite bands within mantle peridotites. The pe...
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| Publicado en: | Boletín de la Sociedad Geológica Mexicana |
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| Principais autores: | , , , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado: |
Sociedad Geológica Mexicana, A.C.
2020
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| Assuntos: | |
| Acceso en liña: | https://www.redalyc.org/articulo.oa?id=94370787003 |
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