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dc.contributor.author
Fogliata, Ana Silvia
dc.contributor.author
Báez, Miguel Adolfo
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Hagemann, S. G.
dc.contributor.author
Santos, O.
dc.contributor.author
Sardi, Fernando Guillermo
dc.date.available
2019-11-22T13:56:54Z
dc.date.issued
2012-06
dc.identifier.citation
Fogliata, Ana Silvia; Báez, Miguel Adolfo; Hagemann, S. G.; Santos, O.; Sardi, Fernando Guillermo; Post-orogenic, Carboniferous granite hosted Sn-W mineralization in the Sierras Pampeanas Orogen, North-western Argentina.; Elsevier Science; Ore Geology Reviews; 45; 6-2012; 16-32
dc.identifier.issn
0169-1368
dc.identifier.uri
http://hdl.handle.net/11336/89523
dc.description.abstract
The Sierras Pampeanas orogen, in northwestern Argentina, hosts significant Sn-W mineralization in a variety of mostly epizonal granite stocks emplaced in variably metamorphosed country rocks. The San Blas, Huaco and El Durazno granite stocks in the Sierra de Velasco, the La Quebrada granite in the Sierra de Mazán, the Cerro Colorado granite in the Cerro Negro, and the Los Mudaderos and Sauce Guacho granite stocks in the Sierra de Ancasti, are largely peraluminous (ASI between 1.05 and 1.38) and represent S-type granites, are strongly fractionated (i.e., high Rb/Sr ratio), have a low oxidation state (low Fe2O3/FeO ratio) and are geotectonically linked to syncollisional magmatism. The U-Pb SHRIMP analyses on zircons from the Cerro Colorado and La Quebrada granites, located in the Cerro Negro and Sierra de Mazán, respectively, revealed ages from Lower Ordovician (Tremadocian) to Carboniferous. All granites display elevated LREE values, low HREE values and negative Eu anomalies. With regards to total REE values, two groups of granite stocks can be recognized. The granites with lower REE contents are highly evolved granites and are related to Sn-W mineralization. The mineralized granites display higher values of Sn, W and Rb, and lower values of Sr and Ba compared to barren granites. These trace element characteristics appear to be diagnostic for Sn-W mineralized granite stocks in the western Sierras Pampeanas. The western Sierras Pampeanas contains locally geochemically evolved Carboniferous granites, which are interpreted to be the main control of significant Sn-W mineralization. The Carboniferous age of western Sierras Pampeanas Sn-W mineralization sets it apart from the Triassic age of the Sn?W mineralization in the Eastern Tin belt of Bolivia.
dc.format
application/pdf
dc.language.iso
eng
dc.publisher
Elsevier Science
dc.rights
info:eu-repo/semantics/openAccess
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.subject
Sn - W Mineralization
dc.subject
Sierras Pampeanas
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Granites
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Argentina
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Geología
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Ciencias de la Tierra y relacionadas con el Medio Ambiente
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CIENCIAS NATURALES Y EXACTAS
dc.title
Post-orogenic, Carboniferous granite hosted Sn-W mineralization in the Sierras Pampeanas Orogen, North-western Argentina.
dc.type
info:eu-repo/semantics/article
dc.type
info:ar-repo/semantics/artículo
dc.type
info:eu-repo/semantics/publishedVersion
dc.date.updated
2019-06-04T16:01:40Z
dc.journal.volume
45
dc.journal.pagination
16-32
dc.journal.pais
Australia
dc.journal.ciudad
Melbourne
dc.description.fil
Fil: Fogliata, Ana Silvia. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Cátedra de Geología de Minas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina
dc.description.fil
Fil: Báez, Miguel Adolfo. Fundación Miguel Lillo; Argentina
dc.description.fil
Fil: Hagemann, S. G.. Universidad Nacional de Tucuman. Facultad de Cs.naturales E Instituto Miguel Lillo. Departamento de Geología; Argentina
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Fil: Santos, O.. University of Western Australia; Australia
dc.description.fil
Fil: Sardi, Fernando Guillermo. University of Western Australia; Australia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología. Cátedra Geología Estructural. Instituto Superior de Correlación Geológica; Argentina
dc.journal.title
Ore Geology Reviews
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/https://dx.doi.org/10.1016/j.oregeorev.2011.12.001
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0169136812000029?via%3Dihub
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