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
.jpg)
- Institución
- Universidad Nacional de La Plata
- OAI Identificador
- oai:sedici.unlp.edu.ar:10915/190490
Ver los metadatos del registro completo
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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 |
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2017-08 |
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