Genesis of El Infiernillo Mining district, San Rafael block, Mendoza

El Infiernillo Mining District is located in the San Rafael Block (34°38'20";68°47'37"), province of Mendoza, Argentina. It is a porphyry Cu (Mo) type deposit which is hosted by a volcaniclastic sequence. It develops an alteration halo with a concentric pattern consisting of a ce...

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Autores principales: Gómez, A., Rubinstein, N.
Formato: Artículo publishedVersion
Publicado: 2010
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00044822_v67_n2_p231_Gomez
https://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_00044822_v67_n2_p231_Gomez_oai
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spelling I28-R145-paper_00044822_v67_n2_p231_Gomez_oai2024-08-16 Gómez, A. Rubinstein, N. 2010 El Infiernillo Mining District is located in the San Rafael Block (34°38'20";68°47'37"), province of Mendoza, Argentina. It is a porphyry Cu (Mo) type deposit which is hosted by a volcaniclastic sequence. It develops an alteration halo with a concentric pattern consisting of a central quartz neck surrounded by a potassic alteration zone and outwards a phyllic halo and small polymetallic veins. The potassic halo has a paragenesis of K-feldspar-quartz-(biotite). Three silicification phases are related to this alteration stage, one of them (with temperature between 550° and 390°C and salinity between 35 and 47 %) genetically linked to the copper mineralization. The phyllic alteration consists of quartz-illite-(rutile) with minor albite. The albitization process points out to an early phase of this phyllic stage. The fluid inclusions together with the textures of the quartz neck suggest the shallowing of the active hydrothermal system. The disseminated ore paragenesis consists of bornite, chalcopyrite-molibdenite, pyrite, (galena-sphalerite). The presence of molibdenite-quartz veins indicate the transition from the potassic to the phyllic stage while the pyrite-quartz ones point out to a transition to a fragile deformation regime during which the polymetallic veins, with a paragenesis of chalcopyrite- sphalerite, pyrite, (Ag) tetrahedrite, galena were formed. The petrologic characteristics of the volcaniclastic host rocks reveal that they correspond to the lower section of Choiyoi magmatic cycle. The magmatic and structural controls constrain the age of this ore deposit to the Early-Middle to Late Permian. Fil:Gómez, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Rubinstein, N. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. application/pdf http://hdl.handle.net/20.500.12110/paper_00044822_v67_n2_p231_Gomez info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar Rev. Asoc. Geol. Argent. 2010;67(2):231-238 Choiyoi magmatic cycle Cu (Mo) porphyry Genesis Lower section copper feldspar fluid inclusion hydrothermal system mineralization molybdenum ore deposit petrogenesis porphyry quartz vein salinity Argentina Mendoza San Rafael [Mendoza] Genesis of El Infiernillo Mining district, San Rafael block, Mendoza info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion https://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_00044822_v67_n2_p231_Gomez_oai
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-145
collection Repositorio Digital de la Universidad de Buenos Aires (UBA)
topic Choiyoi magmatic cycle
Cu (Mo) porphyry
Genesis
Lower section
copper
feldspar
fluid inclusion
hydrothermal system
mineralization
molybdenum
ore deposit
petrogenesis
porphyry
quartz vein
salinity
Argentina
Mendoza
San Rafael [Mendoza]
spellingShingle Choiyoi magmatic cycle
Cu (Mo) porphyry
Genesis
Lower section
copper
feldspar
fluid inclusion
hydrothermal system
mineralization
molybdenum
ore deposit
petrogenesis
porphyry
quartz vein
salinity
Argentina
Mendoza
San Rafael [Mendoza]
Gómez, A.
Rubinstein, N.
Genesis of El Infiernillo Mining district, San Rafael block, Mendoza
topic_facet Choiyoi magmatic cycle
Cu (Mo) porphyry
Genesis
Lower section
copper
feldspar
fluid inclusion
hydrothermal system
mineralization
molybdenum
ore deposit
petrogenesis
porphyry
quartz vein
salinity
Argentina
Mendoza
San Rafael [Mendoza]
description El Infiernillo Mining District is located in the San Rafael Block (34°38'20";68°47'37"), province of Mendoza, Argentina. It is a porphyry Cu (Mo) type deposit which is hosted by a volcaniclastic sequence. It develops an alteration halo with a concentric pattern consisting of a central quartz neck surrounded by a potassic alteration zone and outwards a phyllic halo and small polymetallic veins. The potassic halo has a paragenesis of K-feldspar-quartz-(biotite). Three silicification phases are related to this alteration stage, one of them (with temperature between 550° and 390°C and salinity between 35 and 47 %) genetically linked to the copper mineralization. The phyllic alteration consists of quartz-illite-(rutile) with minor albite. The albitization process points out to an early phase of this phyllic stage. The fluid inclusions together with the textures of the quartz neck suggest the shallowing of the active hydrothermal system. The disseminated ore paragenesis consists of bornite, chalcopyrite-molibdenite, pyrite, (galena-sphalerite). The presence of molibdenite-quartz veins indicate the transition from the potassic to the phyllic stage while the pyrite-quartz ones point out to a transition to a fragile deformation regime during which the polymetallic veins, with a paragenesis of chalcopyrite- sphalerite, pyrite, (Ag) tetrahedrite, galena were formed. The petrologic characteristics of the volcaniclastic host rocks reveal that they correspond to the lower section of Choiyoi magmatic cycle. The magmatic and structural controls constrain the age of this ore deposit to the Early-Middle to Late Permian.
format Artículo
Artículo
publishedVersion
author Gómez, A.
Rubinstein, N.
author_facet Gómez, A.
Rubinstein, N.
author_sort Gómez, A.
title Genesis of El Infiernillo Mining district, San Rafael block, Mendoza
title_short Genesis of El Infiernillo Mining district, San Rafael block, Mendoza
title_full Genesis of El Infiernillo Mining district, San Rafael block, Mendoza
title_fullStr Genesis of El Infiernillo Mining district, San Rafael block, Mendoza
title_full_unstemmed Genesis of El Infiernillo Mining district, San Rafael block, Mendoza
title_sort genesis of el infiernillo mining district, san rafael block, mendoza
publishDate 2010
url http://hdl.handle.net/20.500.12110/paper_00044822_v67_n2_p231_Gomez
https://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_00044822_v67_n2_p231_Gomez_oai
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