Origin and age of rift related fluorite and manganese deposits from the San Rafael Massif, Argentina
The San Rafael Massif is characterized by widespread fluorite and manganese epithermal ore deposits whose origin has been under debate to the present. Isotopic (Sm/Nd and K/Ar) and geochemical (trace elements and REE) data of fluorite and manganese ore allowed to establish the age and genesis of the...
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2015
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| LEADER | 21710caa a22016817a 4500 | ||
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| 001 | PAPER-24813 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205644.0 | ||
| 008 | 190411s2015 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-84920579065 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Rubinstein, N.A. | |
| 245 | 1 | 0 | |a Origin and age of rift related fluorite and manganese deposits from the San Rafael Massif, Argentina |
| 260 | |b Elsevier |c 2015 | ||
| 270 | 1 | 0 | |m Rubinstein, N.A.; Instituto de Geociencias Básicas, Aplicadas y Ambientales (IGEBA, UBA-CONICET) Departamento de Ciencias Geológicas, Pabellón II, Ciudad Universitaria, Argentina |
| 506 | |2 openaire |e Política editorial | ||
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| 504 | |a Zappettini, E.O., Dalponte, M., Segal, S., Cozzi, G., Mineralogía y aspectos genéticos del depósito volcanogénico submarino de manganeso "La Casualidad", Cerro Atravesada, Neuquén (2012) Rev. Asoc. Geol. Argent., 69 (4), pp. 544-555 | ||
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| 520 | 3 | |a The San Rafael Massif is characterized by widespread fluorite and manganese epithermal ore deposits whose origin has been under debate to the present. Isotopic (Sm/Nd and K/Ar) and geochemical (trace elements and REE) data of fluorite and manganese ore allowed to establish the age and genesis of the deposits and to propose a regional genetic model. The fluorite deposits were formed during the Upper Triassic-Lower Jurassic as a result of the Triassic rifting that launched a hydrothermal activity at regional scale. The hydrothermal fluids had low T and high fO2 with fluorine probably derived from a mantle source and REE scavenged from the volcanics of the Gondwanan Choiyoi Magmatic Cycle upper section. The manganese deposits were formed by oxidizing hydrothermal fluids that collected Mn from deep sources and also leached REE from the upper section of the Choiyoi Magmatic Cycle during two mineralization episodes. One episode was linked to the rift tectonic setting that remained active up to the Upper Cretaceous and the other was related to an Early Miocene back-arc extensional geodynamic setting. Both manganese and fluorite deposits were formed in extensional tectonic settings within an epithermal environment near the surface, and can be ascribed to the general model of detachment-related deposits. © 2014 Elsevier B.V. |l eng | |
| 536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas | ||
| 536 | |a Detalles de la financiación: We thank Paula Cornejo Peláez for her cooperation during the isotopic analyses of manganese minerals, Eugenia Fonseca who carried out the XRD determinations, Marcelo Yañez who made the spectrometric analyses, César Vásquez who handled the extraction lines at the SERNAGEOMIN and Anabel Gómez who helped with the figures of this paper. We are grateful to Servicio Geológico Minero Argentino (SEGEMAR) for authorizing the publication of this investigation. This research was partially funded by the PIP 11220090100589, CONICET. | ||
| 593 | |a Instituto de Geociencias Básicas, Aplicadas y Ambientales (IGEBA, UBA-CONICET) Departamento de Ciencias Geológicas, Pabellón II, Ciudad Universitaria, Buenos Aires, C1428EHA, Argentina | ||
| 593 | |a Instituto de Geología y Recursos Minerales, Servicio Geológico Minero Argentino, Avda, General Paz 5445, Edificio 25, Buenos Aires, B1650KNA, Argentina | ||
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a MENDOZA | |
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| 690 | 1 | 0 | |a FLUORITE AND MANGANESE |
| 690 | 1 | 0 | |a ISOTOPES AND GEOCHEMISTRY |
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| 690 | 1 | 0 | |a GEOCHEMICAL METHOD |
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| 700 | 1 | |a Zappettini, E.O. | |
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