Structural control on the distribution of uranium mineralizations of the Choiyoi cycle, San Rafael Massif, Mendoza

Autores
Japas, M.S.; Salvarredi, J.A.; Kleiman, L.E.
Año de publicación
2008
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The main mineralizations of the Sierra Pintada uranium district, San Rafael Massif, Mendoza, are associated with the Choiyoi volcanic province. In the lower section of this magmatic cycle uranium deposits hosted by epiclastic sandstones are predominant. In the upper section, small vein-type deposits of low economic significance are found instead. During the emplacement of these Permian volcanic and sedimentary sequences two different stress regimes, which conditioned the mineralizing systems, were dominant: transpressional (San Rafael orogenic phase) and transtensional (post-orogenic stage). A strain fabric analyses was performed in an attempt to evaluate the control exerted by the structures in the distribution of the uranium mineralizations during these two stages of deformation. So that, a contribution to a better understanding of the genesis of these deposits will aid to the generation of new exploration guides for uranium in the Choiyoi province. In the case of the deposits related to the lower Choiyoi, three orders of magnitude could be defined for the structural control. The fabric of the structures determining the distribution of these mineralizations reflects the structural grain of the San Rafael orogeny. The deposition of uranium hosted by the upper Choiyoi sequences was directly or indirectly influenced by the structures generated under the post-sanrafaelic stress field.
Fil:Japas, M.S. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
Fil:Kleiman, L.E. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
Fuente
Rev. Asoc. Geol. Argent. 2008;63(2):204-212
Materia
Choiyoi
Mineralizations
Permian
San Rafael
Strain fabric
Structural control
deformation mechanism
economic geology
magmatism
mineralization
ore deposit
orogeny
Permian
sandstone
sedimentary sequence
spatial distribution
structural control
transpression
transtension
uranium
Argentina
Mendoza
San Rafael Massif
Sierra Pintada Mine
South America
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by/2.5/ar
Repositorio
Biblioteca Digital (UBA-FCEN)
Institución
Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales
OAI Identificador
paperaa:paper_00044822_v63_n2_p204_Japas

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oai_identifier_str paperaa:paper_00044822_v63_n2_p204_Japas
network_acronym_str BDUBAFCEN
repository_id_str 1896
network_name_str Biblioteca Digital (UBA-FCEN)
spelling Structural control on the distribution of uranium mineralizations of the Choiyoi cycle, San Rafael Massif, Mendoza Japas, M.S.Salvarredi, J.A.Kleiman, L.E.ChoiyoiMineralizationsPermianSan RafaelStrain fabricStructural controldeformation mechanismeconomic geologymagmatismmineralizationore depositorogenyPermiansandstonesedimentary sequencespatial distributionstructural controltranspressiontranstensionuraniumArgentinaMendozaSan Rafael MassifSierra Pintada MineSouth AmericaThe main mineralizations of the Sierra Pintada uranium district, San Rafael Massif, Mendoza, are associated with the Choiyoi volcanic province. In the lower section of this magmatic cycle uranium deposits hosted by epiclastic sandstones are predominant. In the upper section, small vein-type deposits of low economic significance are found instead. During the emplacement of these Permian volcanic and sedimentary sequences two different stress regimes, which conditioned the mineralizing systems, were dominant: transpressional (San Rafael orogenic phase) and transtensional (post-orogenic stage). A strain fabric analyses was performed in an attempt to evaluate the control exerted by the structures in the distribution of the uranium mineralizations during these two stages of deformation. So that, a contribution to a better understanding of the genesis of these deposits will aid to the generation of new exploration guides for uranium in the Choiyoi province. In the case of the deposits related to the lower Choiyoi, three orders of magnitude could be defined for the structural control. The fabric of the structures determining the distribution of these mineralizations reflects the structural grain of the San Rafael orogeny. The deposition of uranium hosted by the upper Choiyoi sequences was directly or indirectly influenced by the structures generated under the post-sanrafaelic stress field.Fil:Japas, M.S. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.Fil:Kleiman, L.E. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.2008info: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_v63_n2_p204_JapasRev. Asoc. Geol. Argent. 2008;63(2):204-212reponame: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/ar2025-09-29T13:43:05Zpaperaa:paper_00044822_v63_n2_p204_JapasInstitucionalhttps://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 13:43:06.972Biblioteca Digital (UBA-FCEN) - Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturalesfalse
dc.title.none.fl_str_mv Structural control on the distribution of uranium mineralizations of the Choiyoi cycle, San Rafael Massif, Mendoza
title Structural control on the distribution of uranium mineralizations of the Choiyoi cycle, San Rafael Massif, Mendoza
spellingShingle Structural control on the distribution of uranium mineralizations of the Choiyoi cycle, San Rafael Massif, Mendoza
Japas, M.S.
Choiyoi
Mineralizations
Permian
San Rafael
Strain fabric
Structural control
deformation mechanism
economic geology
magmatism
mineralization
ore deposit
orogeny
Permian
sandstone
sedimentary sequence
spatial distribution
structural control
transpression
transtension
uranium
Argentina
Mendoza
San Rafael Massif
Sierra Pintada Mine
South America
title_short Structural control on the distribution of uranium mineralizations of the Choiyoi cycle, San Rafael Massif, Mendoza
title_full Structural control on the distribution of uranium mineralizations of the Choiyoi cycle, San Rafael Massif, Mendoza
title_fullStr Structural control on the distribution of uranium mineralizations of the Choiyoi cycle, San Rafael Massif, Mendoza
title_full_unstemmed Structural control on the distribution of uranium mineralizations of the Choiyoi cycle, San Rafael Massif, Mendoza
title_sort Structural control on the distribution of uranium mineralizations of the Choiyoi cycle, San Rafael Massif, Mendoza
dc.creator.none.fl_str_mv Japas, M.S.
Salvarredi, J.A.
Kleiman, L.E.
author Japas, M.S.
author_facet Japas, M.S.
Salvarredi, J.A.
Kleiman, L.E.
author_role author
author2 Salvarredi, J.A.
Kleiman, L.E.
author2_role author
author
dc.subject.none.fl_str_mv Choiyoi
Mineralizations
Permian
San Rafael
Strain fabric
Structural control
deformation mechanism
economic geology
magmatism
mineralization
ore deposit
orogeny
Permian
sandstone
sedimentary sequence
spatial distribution
structural control
transpression
transtension
uranium
Argentina
Mendoza
San Rafael Massif
Sierra Pintada Mine
South America
topic Choiyoi
Mineralizations
Permian
San Rafael
Strain fabric
Structural control
deformation mechanism
economic geology
magmatism
mineralization
ore deposit
orogeny
Permian
sandstone
sedimentary sequence
spatial distribution
structural control
transpression
transtension
uranium
Argentina
Mendoza
San Rafael Massif
Sierra Pintada Mine
South America
dc.description.none.fl_txt_mv The main mineralizations of the Sierra Pintada uranium district, San Rafael Massif, Mendoza, are associated with the Choiyoi volcanic province. In the lower section of this magmatic cycle uranium deposits hosted by epiclastic sandstones are predominant. In the upper section, small vein-type deposits of low economic significance are found instead. During the emplacement of these Permian volcanic and sedimentary sequences two different stress regimes, which conditioned the mineralizing systems, were dominant: transpressional (San Rafael orogenic phase) and transtensional (post-orogenic stage). A strain fabric analyses was performed in an attempt to evaluate the control exerted by the structures in the distribution of the uranium mineralizations during these two stages of deformation. So that, a contribution to a better understanding of the genesis of these deposits will aid to the generation of new exploration guides for uranium in the Choiyoi province. In the case of the deposits related to the lower Choiyoi, three orders of magnitude could be defined for the structural control. The fabric of the structures determining the distribution of these mineralizations reflects the structural grain of the San Rafael orogeny. The deposition of uranium hosted by the upper Choiyoi sequences was directly or indirectly influenced by the structures generated under the post-sanrafaelic stress field.
Fil:Japas, M.S. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
Fil:Kleiman, L.E. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
description The main mineralizations of the Sierra Pintada uranium district, San Rafael Massif, Mendoza, are associated with the Choiyoi volcanic province. In the lower section of this magmatic cycle uranium deposits hosted by epiclastic sandstones are predominant. In the upper section, small vein-type deposits of low economic significance are found instead. During the emplacement of these Permian volcanic and sedimentary sequences two different stress regimes, which conditioned the mineralizing systems, were dominant: transpressional (San Rafael orogenic phase) and transtensional (post-orogenic stage). A strain fabric analyses was performed in an attempt to evaluate the control exerted by the structures in the distribution of the uranium mineralizations during these two stages of deformation. So that, a contribution to a better understanding of the genesis of these deposits will aid to the generation of new exploration guides for uranium in the Choiyoi province. In the case of the deposits related to the lower Choiyoi, three orders of magnitude could be defined for the structural control. The fabric of the structures determining the distribution of these mineralizations reflects the structural grain of the San Rafael orogeny. The deposition of uranium hosted by the upper Choiyoi sequences was directly or indirectly influenced by the structures generated under the post-sanrafaelic stress field.
publishDate 2008
dc.date.none.fl_str_mv 2008
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_v63_n2_p204_Japas
url http://hdl.handle.net/20.500.12110/paper_00044822_v63_n2_p204_Japas
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. 2008;63(2):204-212
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)
collection 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
repository.mail.fl_str_mv ana@bl.fcen.uba.ar
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