The Quebrada del Diablo Lower West Au deposit (Gualcamayo mining district, Argentina): A Carlin-type mineralization?

The Gualcamayo Mining District (GMD), located in the eastern margin of the Argentini an Precordillera includes three Au deposits: Amelia-Ines, Magdalena, Quebrada del Diablo Main, and QDD Lower West. The district has reserves of 491,000 oz. and resources of 2.3 million oz of Au. The metallogenetic a...

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Autor principal: D'Annunzio, M.C
Otros Autores: Rubinstein, N.
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Publicado: Elsevier Ltd 2019
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100 1 |a D'Annunzio, M.C. 
245 1 4 |a The Quebrada del Diablo Lower West Au deposit (Gualcamayo mining district, Argentina): A Carlin-type mineralization? 
260 |b Elsevier Ltd  |c 2019 
270 1 0 |m D'Annunzio, M.C.; INGEOSUR- CONICET- Universidad Nacional del Sur- Departamento de Geología, San Juan 670, Argentina; email: celeste.dannunzio@gmail.com 
506 |2 openaire  |e Política editorial 
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520 3 |a The Gualcamayo Mining District (GMD), located in the eastern margin of the Argentini an Precordillera includes three Au deposits: Amelia-Ines, Magdalena, Quebrada del Diablo Main, and QDD Lower West. The district has reserves of 491,000 oz. and resources of 2.3 million oz of Au. The metallogenetic analysis of these Au deposits based on previous work and new micro-geochemistry (LA- ICP- MS), isotopic (C-O-S-Pb) and fluid inclusions studies revealed that they are genetically linked and share many characteristics with Carlin-type deposits, including the lithology of host rocks, structural control, geochemical signatures, ore paragenesis, and dissolution and decarbonization processes. However, they also display some noticeable differences. The sulfur isotopic composition supports a genetic link between these gold deposits and the precursor magmatism of the porphyry-type mineralization of the area. Besides, the fluids responsible for the Au mineralization proved to be neutral to slightly alkaline and Au-saturated. The link with the magmatism along with the character of the mineralizing fluids and the presence of significant base metal sulfides allowed classifying the GMD deposits as “distal disseminated gold deposits” that occur on the distal edges of magmatic-hydrothermal systems. © 2019 Elsevier Ltd  |l eng 
536 |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas 
536 |a Detalles de la financiación: We thank M.A.S.A. (Minas Argentinas Sociedad Anonima, Yamana Gold) that authorized the field work, sampling and, financed the isotopic analysis. This project was funded by PIP 1220130100107 CO ( CONICET ) project, Argentina. We thank to the reviewers of the manuscript, because their suggestions allowed us to improve it substantially. 
593 |a INGEOSUR- CONICET- Universidad Nacional del Sur- Departamento de Geología, San Juan 670, Bahía Blanca, Argentina 
593 |a IGEBa, Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Pabellón 2, Ciudad Universitaria, Ciudad Autónoma de Buenos Aires, Argentina 
690 1 0 |a CHARACTER OF THE MINERALIZING FLUIDS 
690 1 0 |a DISTAL DISSEMINATED AU DEPOSIT 
690 1 0 |a HOST ROCKS 
690 1 0 |a MAGMATIC ORIGIN 
690 1 0 |a PRECORDILLERA 
690 1 0 |a STRUCTURAL CONTROL 
700 1 |a Rubinstein, N. 
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