Characteristics of Central II alteration zone, San Rafael Massif, province of Mendoza
- Autores
- Gargiulo, M.F.; Rubinstein, N.; Carpio, F.; Salvarredi, J.
- Año de publicación
- 2007
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The goal of this paper is to present the petrographic study from outcrop samples of the Central II alteration zone. This area is located in the San Rafael Massif, province of Mendoza (34°54'56" S; 68°37'02" O) and is related to hypoabyssal rhyolitic bodies that intrude a volcanic-volcaniclastic sequence corresponding to the upper section of Choiyoi Group. The alteration zone is represented by pervasive sericitization overprinted by silicic breccias and veins with WNW trend (Az 290° - 300°) and vertical dip. Hydrothermal veins are mainly composed by quartz with primary growth, recrystalization and replacement textures with minor pyrite, chalcopyrite and scarce arsenopyrite. The combination of crustifiform - colloform silica banding, quartz pseudomorphs of bladed calcite and adularia with different morphologies (sub-rhombic, rhombic and pseudo-acicular) is a clear evidence of a low-sulfidation epithermal system with paleozones of upflow boiling.
Fil:Gargiulo, M.F. 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. - Fuente
- Rev. Asoc. Geol. Argent. 2007;62(3):387-395
- Materia
-
Adularia
Boiling upflow
Hydrothermal quartz
Low-sulfidation epithermal system
Upper section of Choiyoi Group
abyssal zone
epithermal deposit
hydrothermal activity
hydrothermal alteration
hydrothermal system
outcrop
petrography
pseudomorph
recrystallization
rhyolite
Argentina
Mendoza
San Rafael Massif
South America - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- http://creativecommons.org/licenses/by/2.5/ar
- Repositorio
- Institución
- Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales
- OAI Identificador
- paperaa:paper_00044822_v62_n3_p387_Gargiulo
Ver los metadatos del registro completo
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Characteristics of Central II alteration zone, San Rafael Massif, province of Mendoza Gargiulo, M.F.Rubinstein, N.Carpio, F.Salvarredi, J.AdulariaBoiling upflowHydrothermal quartzLow-sulfidation epithermal systemUpper section of Choiyoi Groupabyssal zoneepithermal deposithydrothermal activityhydrothermal alterationhydrothermal systemoutcroppetrographypseudomorphrecrystallizationrhyoliteArgentinaMendozaSan Rafael MassifSouth AmericaThe goal of this paper is to present the petrographic study from outcrop samples of the Central II alteration zone. This area is located in the San Rafael Massif, province of Mendoza (34°54'56" S; 68°37'02" O) and is related to hypoabyssal rhyolitic bodies that intrude a volcanic-volcaniclastic sequence corresponding to the upper section of Choiyoi Group. The alteration zone is represented by pervasive sericitization overprinted by silicic breccias and veins with WNW trend (Az 290° - 300°) and vertical dip. Hydrothermal veins are mainly composed by quartz with primary growth, recrystalization and replacement textures with minor pyrite, chalcopyrite and scarce arsenopyrite. The combination of crustifiform - colloform silica banding, quartz pseudomorphs of bladed calcite and adularia with different morphologies (sub-rhombic, rhombic and pseudo-acicular) is a clear evidence of a low-sulfidation epithermal system with paleozones of upflow boiling.Fil:Gargiulo, M.F. 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.2007info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfhttp://hdl.handle.net/20.500.12110/paper_00044822_v62_n3_p387_GargiuloRev. Asoc. Geol. Argent. 2007;62(3):387-395reponame:Biblioteca Digital (UBA-FCEN)instname:Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturalesinstacron:UBA-FCENenginfo:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by/2.5/ar2025-09-29T13:42:52Zpaperaa:paper_00044822_v62_n3_p387_GargiuloInstitucionalhttps://digital.bl.fcen.uba.ar/Universidad públicaNo correspondehttps://digital.bl.fcen.uba.ar/cgi-bin/oaiserver.cgiana@bl.fcen.uba.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:18962025-09-29 13:42:53.409Biblioteca Digital (UBA-FCEN) - Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturalesfalse |
dc.title.none.fl_str_mv |
Characteristics of Central II alteration zone, San Rafael Massif, province of Mendoza |
title |
Characteristics of Central II alteration zone, San Rafael Massif, province of Mendoza |
spellingShingle |
Characteristics of Central II alteration zone, San Rafael Massif, province of Mendoza Gargiulo, M.F. Adularia Boiling upflow Hydrothermal quartz Low-sulfidation epithermal system Upper section of Choiyoi Group abyssal zone epithermal deposit hydrothermal activity hydrothermal alteration hydrothermal system outcrop petrography pseudomorph recrystallization rhyolite Argentina Mendoza San Rafael Massif South America |
title_short |
Characteristics of Central II alteration zone, San Rafael Massif, province of Mendoza |
title_full |
Characteristics of Central II alteration zone, San Rafael Massif, province of Mendoza |
title_fullStr |
Characteristics of Central II alteration zone, San Rafael Massif, province of Mendoza |
title_full_unstemmed |
Characteristics of Central II alteration zone, San Rafael Massif, province of Mendoza |
title_sort |
Characteristics of Central II alteration zone, San Rafael Massif, province of Mendoza |
dc.creator.none.fl_str_mv |
Gargiulo, M.F. Rubinstein, N. Carpio, F. Salvarredi, J. |
author |
Gargiulo, M.F. |
author_facet |
Gargiulo, M.F. Rubinstein, N. Carpio, F. Salvarredi, J. |
author_role |
author |
author2 |
Rubinstein, N. Carpio, F. Salvarredi, J. |
author2_role |
author author author |
dc.subject.none.fl_str_mv |
Adularia Boiling upflow Hydrothermal quartz Low-sulfidation epithermal system Upper section of Choiyoi Group abyssal zone epithermal deposit hydrothermal activity hydrothermal alteration hydrothermal system outcrop petrography pseudomorph recrystallization rhyolite Argentina Mendoza San Rafael Massif South America |
topic |
Adularia Boiling upflow Hydrothermal quartz Low-sulfidation epithermal system Upper section of Choiyoi Group abyssal zone epithermal deposit hydrothermal activity hydrothermal alteration hydrothermal system outcrop petrography pseudomorph recrystallization rhyolite Argentina Mendoza San Rafael Massif South America |
dc.description.none.fl_txt_mv |
The goal of this paper is to present the petrographic study from outcrop samples of the Central II alteration zone. This area is located in the San Rafael Massif, province of Mendoza (34°54'56" S; 68°37'02" O) and is related to hypoabyssal rhyolitic bodies that intrude a volcanic-volcaniclastic sequence corresponding to the upper section of Choiyoi Group. The alteration zone is represented by pervasive sericitization overprinted by silicic breccias and veins with WNW trend (Az 290° - 300°) and vertical dip. Hydrothermal veins are mainly composed by quartz with primary growth, recrystalization and replacement textures with minor pyrite, chalcopyrite and scarce arsenopyrite. The combination of crustifiform - colloform silica banding, quartz pseudomorphs of bladed calcite and adularia with different morphologies (sub-rhombic, rhombic and pseudo-acicular) is a clear evidence of a low-sulfidation epithermal system with paleozones of upflow boiling. Fil:Gargiulo, M.F. 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. |
description |
The goal of this paper is to present the petrographic study from outcrop samples of the Central II alteration zone. This area is located in the San Rafael Massif, province of Mendoza (34°54'56" S; 68°37'02" O) and is related to hypoabyssal rhyolitic bodies that intrude a volcanic-volcaniclastic sequence corresponding to the upper section of Choiyoi Group. The alteration zone is represented by pervasive sericitization overprinted by silicic breccias and veins with WNW trend (Az 290° - 300°) and vertical dip. Hydrothermal veins are mainly composed by quartz with primary growth, recrystalization and replacement textures with minor pyrite, chalcopyrite and scarce arsenopyrite. The combination of crustifiform - colloform silica banding, quartz pseudomorphs of bladed calcite and adularia with different morphologies (sub-rhombic, rhombic and pseudo-acicular) is a clear evidence of a low-sulfidation epithermal system with paleozones of upflow boiling. |
publishDate |
2007 |
dc.date.none.fl_str_mv |
2007 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://hdl.handle.net/20.500.12110/paper_00044822_v62_n3_p387_Gargiulo |
url |
http://hdl.handle.net/20.500.12110/paper_00044822_v62_n3_p387_Gargiulo |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
http://creativecommons.org/licenses/by/2.5/ar |
dc.format.none.fl_str_mv |
application/pdf |
dc.source.none.fl_str_mv |
Rev. Asoc. Geol. Argent. 2007;62(3):387-395 reponame:Biblioteca Digital (UBA-FCEN) instname:Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales instacron:UBA-FCEN |
reponame_str |
Biblioteca Digital (UBA-FCEN) |
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Biblioteca Digital (UBA-FCEN) |
instname_str |
Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales |
instacron_str |
UBA-FCEN |
institution |
UBA-FCEN |
repository.name.fl_str_mv |
Biblioteca Digital (UBA-FCEN) - Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales |
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ana@bl.fcen.uba.ar |
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