Petrography, geochemistry and geochronology of San Jorge porphyry Cu-Au deposit, Mendoza, Argentina. Constraints for the timing of magmatism and associated mineralization
The San Jorge porphyry Cu-Au deposit, Argentina, integrates the Paleozoic to Early Jurassic metallogenic belt recognized in the Southern Andes. San Jorge is currently the only deposit considered economically viable due to its supergene enrichment. Previous studies have reported Middle to Upper Permian ages (257-270 Ma) for the intrusion-mineralization processes. Granite porphyry, two granodiorite porphyries (G1 and G2) and an alkali-feldspar granite dike were recognized. These granites intrude sedimentary rocks (Yalguaráz Formation) that hosts the main mineralization. Two tourmaline alteration events occurred prior to the potassic episode. They are overprinted by phyllic alteration that has an elongated shape with potassic mineralized cores. The mineralization is linked to the potassic alteration in the sedi- mentary sequence and in the granite porphyry that has the highest Cu contents (1% to 3%). The phyllic alteration has pyrrhotite, arsenopyrite and minor chalcopyrite. Digenite, chalcocite and covellite appear in the supergene; malachite and brochantite in the oxide; and goethite, hematite and jarosite in gossan zones. The granitic porphyry, granodiorite porphyries G1 and two potassic alteration biotites are of Early Permian age. This event produces the potassic alteration and mineralization and is 15 Ma older than the ages determined by other authors. The granodiorite porphyry G2 and the alkali feldspar granite dike are Upper Permian in age. The results suggest that the evolu- tion of the western margin of Gondwana began in late Carboniferous and continued during the Permian period. In this Paleozoic to early Jurassic metallogenic belt, La Voluntad Cu-Mo porphyry is the oldest deposit (early Pennsylvanian, Garrido et al. 2008). Mineralized and no mineralized San Jorge granites (Early Permian-Late Permian) integrate the intrusive event of the Choiyoi Group
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2018
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Garrido, Mirta M. Grecco, Laura E. Gonzalez, María V. Pavon Pivetta, Cecilia M. |
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Garrido, Mirta M. Grecco, Laura E. Gonzalez, María V. Pavon Pivetta, Cecilia M. Petrography, geochemistry and geochronology of San Jorge porphyry Cu-Au deposit, Mendoza, Argentina. Constraints for the timing of magmatism and associated mineralization |
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Garrido, Mirta M. Grecco, Laura E. Gonzalez, María V. Pavon Pivetta, Cecilia M. |
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Garrido, Mirta M. |
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Petrography, geochemistry and geochronology of San Jorge porphyry Cu-Au deposit, Mendoza, Argentina. Constraints for the timing of magmatism and associated mineralization |
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Petrography, geochemistry and geochronology of San Jorge porphyry Cu-Au deposit, Mendoza, Argentina. Constraints for the timing of magmatism and associated mineralization |
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Petrography, geochemistry and geochronology of San Jorge porphyry Cu-Au deposit, Mendoza, Argentina. Constraints for the timing of magmatism and associated mineralization |
title_fullStr |
Petrography, geochemistry and geochronology of San Jorge porphyry Cu-Au deposit, Mendoza, Argentina. Constraints for the timing of magmatism and associated mineralization |
title_full_unstemmed |
Petrography, geochemistry and geochronology of San Jorge porphyry Cu-Au deposit, Mendoza, Argentina. Constraints for the timing of magmatism and associated mineralization |
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petrography, geochemistry and geochronology of san jorge porphyry cu-au deposit, mendoza, argentina. constraints for the timing of magmatism and associated mineralization |
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The San Jorge porphyry Cu-Au deposit, Argentina, integrates the Paleozoic to Early Jurassic metallogenic belt recognized in the Southern Andes. San Jorge is currently the only deposit considered economically viable due to its supergene enrichment. Previous studies have reported Middle to Upper Permian ages (257-270 Ma) for the intrusion-mineralization processes. Granite porphyry, two granodiorite porphyries (G1 and G2) and an alkali-feldspar granite dike were recognized. These granites intrude sedimentary rocks (Yalguaráz Formation) that hosts the main mineralization. Two tourmaline alteration events occurred prior to the potassic episode. They are overprinted by phyllic alteration that has an elongated shape with potassic mineralized cores. The mineralization is linked to the potassic alteration in the sedi- mentary sequence and in the granite porphyry that has the highest Cu contents (1% to 3%). The phyllic alteration has pyrrhotite, arsenopyrite and minor chalcopyrite. Digenite, chalcocite and covellite appear in the supergene; malachite and brochantite in the oxide; and goethite, hematite and jarosite in gossan zones.
The granitic porphyry, granodiorite porphyries G1 and two potassic alteration biotites are of Early Permian age. This event produces the potassic alteration and mineralization and is 15 Ma older than the ages determined by other authors. The granodiorite porphyry G2 and the alkali feldspar granite dike are Upper Permian in age. The results suggest that the evolu- tion of the western margin of Gondwana began in late Carboniferous and continued during the Permian period. In this Paleozoic to early Jurassic metallogenic belt, La Voluntad Cu-Mo porphyry is the oldest deposit (early Pennsylvanian, Garrido et al. 2008). Mineralized and no mineralized San Jorge granites (Early Permian-Late Permian) integrate the intrusive event of the Choiyoi Group |
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Fundación Miguel Lillo |
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http://www.lillo.org.ar/journals/index.php/acta-geologica-lilloana/article/view/v30n1a01 |
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rev-actageologica-ar-article-322018-10-08T15:16:47Z Petrography, geochemistry and geochronology of San Jorge porphyry Cu-Au deposit, Mendoza, Argentina. Constraints for the timing of magmatism and associated mineralization Petrografía, geoquímica y geocronología del pórfido Cu-Au San Jorge, Mendoza, Argentina. Límites para el magmatismo y la mineralización asociada Garrido, Mirta M. Grecco, Laura E. Gonzalez, María V. Pavon Pivetta, Cecilia M. Depósito de Cu-Au San Jorge petrografía geoquímica geocronología de 40Ar/39 Ar y U-Pb San Jorge copper-gold deposit petrography geochemistry geochronology 40Ar/39 Ar and U-Pb The San Jorge porphyry Cu-Au deposit, Argentina, integrates the Paleozoic to Early Jurassic metallogenic belt recognized in the Southern Andes. San Jorge is currently the only deposit considered economically viable due to its supergene enrichment. Previous studies have reported Middle to Upper Permian ages (257-270 Ma) for the intrusion-mineralization processes. Granite porphyry, two granodiorite porphyries (G1 and G2) and an alkali-feldspar granite dike were recognized. These granites intrude sedimentary rocks (Yalguaráz Formation) that hosts the main mineralization. Two tourmaline alteration events occurred prior to the potassic episode. They are overprinted by phyllic alteration that has an elongated shape with potassic mineralized cores. The mineralization is linked to the potassic alteration in the sedi- mentary sequence and in the granite porphyry that has the highest Cu contents (1% to 3%). The phyllic alteration has pyrrhotite, arsenopyrite and minor chalcopyrite. Digenite, chalcocite and covellite appear in the supergene; malachite and brochantite in the oxide; and goethite, hematite and jarosite in gossan zones. The granitic porphyry, granodiorite porphyries G1 and two potassic alteration biotites are of Early Permian age. This event produces the potassic alteration and mineralization and is 15 Ma older than the ages determined by other authors. The granodiorite porphyry G2 and the alkali feldspar granite dike are Upper Permian in age. The results suggest that the evolu- tion of the western margin of Gondwana began in late Carboniferous and continued during the Permian period. In this Paleozoic to early Jurassic metallogenic belt, La Voluntad Cu-Mo porphyry is the oldest deposit (early Pennsylvanian, Garrido et al. 2008). Mineralized and no mineralized San Jorge granites (Early Permian-Late Permian) integrate the intrusive event of the Choiyoi Group “Petrografía, geoquímica y geocronología del pórfido Cu-Au San Jorge, Mendoza, Argentina. Límites para el magmatismo y la mineralización asociada”. El depósito de pórfido Cu-Au de San Jorge, Argentina, integra el cinturón metalogénico del Paleozoico al Jurásico Temprano, reconocido en los Andes del Sur. San Jorge es actualmente el único depósito considerado económicamente viable debido a su enriquecimiento supergénico. Estu- dios previos dieron edades del Pérmico Medio a Superior (257-270 Ma) para los procesos de intrusión-mineralización. Se reconocieron pórfidos de granito, dos pórfidos de granodiorita (G1 y G2) y un dique de granito alcali-feldespático. Estos granitos intruyen rocas sedimentarias (Formación Yalguaráz) que alberga la principal mineralización. Dos eventos de turmalinización ocurrieron previos al episodio potásico. Están sobreimpuestos por una alteración fílica que tiene una forma elongada con núcleos mineralizados potásicos. La mineralización está ligada a la alteración potásica en la secuencia sedimentaria y en el pórfido de granito que tiene los mayores contenidos de Cu (1% a 3%). La alteración fílica contiene pirrotina, arsenopirita y menor calcopirita. Digenita, calcosina y covelina aparecen en la zona supergénica; malaquita y brochantita en la de óxidos; y goethita, hematita y jarosita en las zonas gossan. El pórfido granítico, el pórfido de granodiorita G1 y dos biotitas de alteración potásica son de edad Pérmico inferior. Este evento produce alteración potásica y mineralización y tiene 15 Ma más que las edades determinadas por otros autores. El pórfido de granodiorita G2 y el dique de granito álcali-feldespático son de edad Pérmico superior. Se propone un mínimo de 2 Ma de edad para la duración del sistema hidrotermal. Los resultados sugieren que la evolución del margen occidental de Gondwana comenzó a finales del Carbonífero y continuó durante el período Pérmico. En este cinturón metalogénico del Paleozoico al Jurásico Temprano, el pórfido La Voluntad Cu-Mo es el depósito más antiguo (Pensilvaniano temprano, Garrido et al., 2008). Los granitos mineralizados y no mineralizados de San Jorge (Pérmico Temprano-Pérmico Superior) integran el evento intrusivo del Grupo Choiyoi. Fundación Miguel Lillo 2018-06-07 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Artículo revisado por pares http://www.lillo.org.ar/journals/index.php/acta-geologica-lilloana/article/view/v30n1a01 Acta Geológica Lilloana; Acta Geológica Lilloana 30 (1) (2018); 1-22 1852-6217 eng http://www.lillo.org.ar/journals/index.php/acta-geologica-lilloana/article/view/v30n1a01/38 http://www.lillo.org.ar/journals/index.php/acta-geologica-lilloana/article/view/v30n1a01/39 |