El enjambre. Ejemplo de un depósito estratoligado de celestina en el norte de la provincia del Neuquén

Autores
Blanco, Miguel Ángel del; Zuazo, Jerónimo Juan
Año de publicación
2017
Idioma
español castellano
Tipo de recurso
documento de conferencia
Estado
versión publicada
Descripción
In this paper, the main features geological characteristics ofthe Sr ore deposit El Enjambre are presented. lt is situated in the northem sector ofthe Neuquén province. The El Enjambre mine is a stratabound deposit related to the Huitrín Formation. lt which constitutes a stratiform mineralization of celestite which shows with replacement evidences features. Celestite replaces anhidryte-gypsum beds with later calcitization processes. Pyrite appears as cavity coatings inside the mineralized manto. This feature allows establish sorne similarities with the Sr-ore deposits ofNaunauco-Taquimilán sector, a few kilometers to the west. lt propose a replacement origin for the El Enjambre mine over gypsum - anhydrite layers by hydrothermal fluids witch carried so4= and Sr possibly produced by thermal action oftertiary magmatism.
Facultad de Ciencias Naturales y Museo
Instituto de Recursos Minerales
Materia
Geología
Celestite
Gypsum
Replacement
Huitrin Formation
Celestina
Yeso
Reemplazo
Formación Huitrín
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by-nc-sa/4.0/
Repositorio
SEDICI (UNLP)
Institución
Universidad Nacional de La Plata
OAI Identificador
oai:sedici.unlp.edu.ar:10915/190490

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oai_identifier_str oai:sedici.unlp.edu.ar:10915/190490
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repository_id_str 1329
network_name_str SEDICI (UNLP)
spelling El enjambre. Ejemplo de un depósito estratoligado de celestina en el norte de la provincia del NeuquénEl Enjambre. Example of a stratoligated celestite deposit in the north of the province of NeuquénBlanco, Miguel Ángel delZuazo, Jerónimo JuanGeologíaCelestiteGypsumReplacementHuitrin FormationCelestinaYesoReemplazoFormación HuitrínIn this paper, the main features geological characteristics ofthe Sr ore deposit El Enjambre are presented. lt is situated in the northem sector ofthe Neuquén province. The El Enjambre mine is a stratabound deposit related to the Huitrín Formation. lt which constitutes a stratiform mineralization of celestite which shows with replacement evidences features. Celestite replaces anhidryte-gypsum beds with later calcitization processes. Pyrite appears as cavity coatings inside the mineralized manto. This feature allows establish sorne similarities with the Sr-ore deposits ofNaunauco-Taquimilán sector, a few kilometers to the west. lt propose a replacement origin for the El Enjambre mine over gypsum - anhydrite layers by hydrothermal fluids witch carried so4= and Sr possibly produced by thermal action oftertiary magmatism.Facultad de Ciencias Naturales y MuseoInstituto de Recursos Minerales2017-08info:eu-repo/semantics/conferenceObjectinfo:eu-repo/semantics/publishedVersionResumenhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdf39-40http://sedici.unlp.edu.ar/handle/10915/190490spainfo:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-sa/4.0/Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2026-02-26T11:39:56Zoai:sedici.unlp.edu.ar:10915/190490Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292026-02-26 11:39:56.589SEDICI (UNLP) - Universidad Nacional de La Platafalse
dc.title.none.fl_str_mv El enjambre. Ejemplo de un depósito estratoligado de celestina en el norte de la provincia del Neuquén
El Enjambre. Example of a stratoligated celestite deposit in the north of the province of Neuquén
title El enjambre. Ejemplo de un depósito estratoligado de celestina en el norte de la provincia del Neuquén
spellingShingle El enjambre. Ejemplo de un depósito estratoligado de celestina en el norte de la provincia del Neuquén
Blanco, Miguel Ángel del
Geología
Celestite
Gypsum
Replacement
Huitrin Formation
Celestina
Yeso
Reemplazo
Formación Huitrín
title_short El enjambre. Ejemplo de un depósito estratoligado de celestina en el norte de la provincia del Neuquén
title_full El enjambre. Ejemplo de un depósito estratoligado de celestina en el norte de la provincia del Neuquén
title_fullStr El enjambre. Ejemplo de un depósito estratoligado de celestina en el norte de la provincia del Neuquén
title_full_unstemmed El enjambre. Ejemplo de un depósito estratoligado de celestina en el norte de la provincia del Neuquén
title_sort El enjambre. Ejemplo de un depósito estratoligado de celestina en el norte de la provincia del Neuquén
dc.creator.none.fl_str_mv Blanco, Miguel Ángel del
Zuazo, Jerónimo Juan
author Blanco, Miguel Ángel del
author_facet Blanco, Miguel Ángel del
Zuazo, Jerónimo Juan
author_role author
author2 Zuazo, Jerónimo Juan
author2_role author
dc.subject.none.fl_str_mv Geología
Celestite
Gypsum
Replacement
Huitrin Formation
Celestina
Yeso
Reemplazo
Formación Huitrín
topic Geología
Celestite
Gypsum
Replacement
Huitrin Formation
Celestina
Yeso
Reemplazo
Formación Huitrín
dc.description.none.fl_txt_mv In this paper, the main features geological characteristics ofthe Sr ore deposit El Enjambre are presented. lt is situated in the northem sector ofthe Neuquén province. The El Enjambre mine is a stratabound deposit related to the Huitrín Formation. lt which constitutes a stratiform mineralization of celestite which shows with replacement evidences features. Celestite replaces anhidryte-gypsum beds with later calcitization processes. Pyrite appears as cavity coatings inside the mineralized manto. This feature allows establish sorne similarities with the Sr-ore deposits ofNaunauco-Taquimilán sector, a few kilometers to the west. lt propose a replacement origin for the El Enjambre mine over gypsum - anhydrite layers by hydrothermal fluids witch carried so4= and Sr possibly produced by thermal action oftertiary magmatism.
Facultad de Ciencias Naturales y Museo
Instituto de Recursos Minerales
description In this paper, the main features geological characteristics ofthe Sr ore deposit El Enjambre are presented. lt is situated in the northem sector ofthe Neuquén province. The El Enjambre mine is a stratabound deposit related to the Huitrín Formation. lt which constitutes a stratiform mineralization of celestite which shows with replacement evidences features. Celestite replaces anhidryte-gypsum beds with later calcitization processes. Pyrite appears as cavity coatings inside the mineralized manto. This feature allows establish sorne similarities with the Sr-ore deposits ofNaunauco-Taquimilán sector, a few kilometers to the west. lt propose a replacement origin for the El Enjambre mine over gypsum - anhydrite layers by hydrothermal fluids witch carried so4= and Sr possibly produced by thermal action oftertiary magmatism.
publishDate 2017
dc.date.none.fl_str_mv 2017-08
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info:eu-repo/semantics/publishedVersion
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status_str publishedVersion
dc.identifier.none.fl_str_mv http://sedici.unlp.edu.ar/handle/10915/190490
url http://sedici.unlp.edu.ar/handle/10915/190490
dc.language.none.fl_str_mv spa
language spa
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
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Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)
eu_rights_str_mv openAccess
rights_invalid_str_mv http://creativecommons.org/licenses/by-nc-sa/4.0/
Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)
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