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
- Institución
- Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales
- OAI Identificador
- paperaa:paper_00044822_v63_n2_p204_Japas
Ver los metadatos del registro completo
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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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1844618739027279872 |
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13.070432 |