Chemical and mineralogical profile of the Las Águilas mafic-ultramafic drill core, San Luis Province, Argentina
Mafic-ultramafic rocks (M-UM) outcropping in the Sierras constitute a 3 to 5 km wide belt that extends 100 km NE-SW. The Las Águilas maficultramafic body carry a sulphide mineralization consisting of pyrrhotite, pentlandite, and chalcopyrite, as veins and disseminated to massive ore. Associated with...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2005 |
| País: | Argentina |
| Institución: | Consejo Nacional de Investigaciones Científicas y Técnicas |
| Repositorio: | CONICET Digital (CONICET) |
| Idioma: | inglés |
| OAI Identifier: | oai:ri.conicet.gov.ar:11336/78114 |
| Acceso en línea: | http://hdl.handle.net/11336/78114 |
| Access Level: | acceso abierto |
| Palabra clave: | https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
| Sumario: | Mafic-ultramafic rocks (M-UM) outcropping in the Sierras constitute a 3 to 5 km wide belt that extends 100 km NE-SW. The Las Águilas maficultramafic body carry a sulphide mineralization consisting of pyrrhotite, pentlandite, and chalcopyrite, as veins and disseminated to massive ore. Associated with the sulphide minerals are disseminated chromites (spl) and platinum group minerals (PGM) such as Pdbismuthotellurides (merenskyite), platinum arsenides (sperrylite). Drill cores from Las Aguilas indicate that mafic units (norite-gabbronorites) dominate in the upper part with ultramafic units (pyroxenites-websterites and dunites-harzburgites) become more significant at depth. A strong correlation between S, Ni, Co, Cu, Cr, Pt and Pd indicates the presence of one to three levels of mineralization within the ultramafic unit. The maximum concentration of these elements coincides with the mineralized units containing PGM and chromite. These relationships reinforce their value as an exploration tool in areas where primary magmatic sulphide mineralizations have been affected by later remobilization processes and the host rocks are tectonically disturbed. |
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