Geology of the Manantial Espejo epithermal district, Deseado Massif, Patagonia Argentina

Autores
Echeveste, Horacio José; López, Luciano; Carlini, Mercedes
Año de publicación
2016
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The silver–gold epithermal mining district, Manantial Espejo, is located southwest of the Deseado Massif, Patagonia. The district is set into Jurassic volcaniclastic rocks of the Bahía Laura Group. A geological map of the district, at a scale of 1:50,000 drawn over a base map prepared from the fusion of satellite imagery and aerial photographs, is included. A suite of andesitic to rhyolitic eruptive units was identified, with prevailing high-grade rhyolitic ignimbrites. Travertine levels show the beginning of a hot-spring system in the region. Quartz veins, with typical crustiform–colloform banded structures, fill WNW, sub-vertical, normal faults, originating from extensional tectonics. The silicification of travertines, tuffs and breccia is the most common hydrothermal alteration.
Facultad de Ciencias Naturales y Museo
Materia
Ciencias Naturales
epithermal
Geology
hot-spring
mining
Patagonia
silver–gold
volcanism
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:10915/85857
Acceder
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network_name_str SEDICI (UNLP)
spelling Geology of the Manantial Espejo epithermal district, Deseado Massif, Patagonia ArgentinaEcheveste, Horacio JoséLópez, LucianoCarlini, MercedesCiencias NaturalesepithermalGeologyhot-springminingPatagoniasilver–goldvolcanismThe silver–gold epithermal mining district, Manantial Espejo, is located southwest of the Deseado Massif, Patagonia. The district is set into Jurassic volcaniclastic rocks of the Bahía Laura Group. A geological map of the district, at a scale of 1:50,000 drawn over a base map prepared from the fusion of satellite imagery and aerial photographs, is included. A suite of andesitic to rhyolitic eruptive units was identified, with prevailing high-grade rhyolitic ignimbrites. Travertine levels show the beginning of a hot-spring system in the region. Quartz veins, with typical crustiform–colloform banded structures, fill WNW, sub-vertical, normal faults, originating from extensional tectonics. The silicification of travertines, tuffs and breccia is the most common hydrothermal alteration.Facultad de Ciencias Naturales y Museo2016info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionArticulohttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdf172-177http://sedici.unlp.edu.ar/handle/10915/85857enginfo:eu-repo/semantics/altIdentifier/issn/1744-5647info:eu-repo/semantics/altIdentifier/doi/10.1080/17445647.2016.1187676info: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:UNLP2025-09-29T11:16:44Zoai:sedici.unlp.edu.ar:10915/85857Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-09-29 11:16:44.554SEDICI (UNLP) - Universidad Nacional de La Platafalse
dc.title.none.fl_str_mv Geology of the Manantial Espejo epithermal district, Deseado Massif, Patagonia Argentina
title Geology of the Manantial Espejo epithermal district, Deseado Massif, Patagonia Argentina
spellingShingle Geology of the Manantial Espejo epithermal district, Deseado Massif, Patagonia Argentina
Echeveste, Horacio José
Ciencias Naturales
epithermal
Geology
hot-spring
mining
Patagonia
silver–gold
volcanism
title_short Geology of the Manantial Espejo epithermal district, Deseado Massif, Patagonia Argentina
title_full Geology of the Manantial Espejo epithermal district, Deseado Massif, Patagonia Argentina
title_fullStr Geology of the Manantial Espejo epithermal district, Deseado Massif, Patagonia Argentina
title_full_unstemmed Geology of the Manantial Espejo epithermal district, Deseado Massif, Patagonia Argentina
title_sort Geology of the Manantial Espejo epithermal district, Deseado Massif, Patagonia Argentina
dc.creator.none.fl_str_mv Echeveste, Horacio José
López, Luciano
Carlini, Mercedes
author Echeveste, Horacio José
author_facet Echeveste, Horacio José
López, Luciano
Carlini, Mercedes
author_role author
author2 López, Luciano
Carlini, Mercedes
author2_role author
author
dc.subject.none.fl_str_mv Ciencias Naturales
epithermal
Geology
hot-spring
mining
Patagonia
silver–gold
volcanism
topic Ciencias Naturales
epithermal
Geology
hot-spring
mining
Patagonia
silver–gold
volcanism
dc.description.none.fl_txt_mv The silver–gold epithermal mining district, Manantial Espejo, is located southwest of the Deseado Massif, Patagonia. The district is set into Jurassic volcaniclastic rocks of the Bahía Laura Group. A geological map of the district, at a scale of 1:50,000 drawn over a base map prepared from the fusion of satellite imagery and aerial photographs, is included. A suite of andesitic to rhyolitic eruptive units was identified, with prevailing high-grade rhyolitic ignimbrites. Travertine levels show the beginning of a hot-spring system in the region. Quartz veins, with typical crustiform–colloform banded structures, fill WNW, sub-vertical, normal faults, originating from extensional tectonics. The silicification of travertines, tuffs and breccia is the most common hydrothermal alteration.
Facultad de Ciencias Naturales y Museo
description The silver–gold epithermal mining district, Manantial Espejo, is located southwest of the Deseado Massif, Patagonia. The district is set into Jurassic volcaniclastic rocks of the Bahía Laura Group. A geological map of the district, at a scale of 1:50,000 drawn over a base map prepared from the fusion of satellite imagery and aerial photographs, is included. A suite of andesitic to rhyolitic eruptive units was identified, with prevailing high-grade rhyolitic ignimbrites. Travertine levels show the beginning of a hot-spring system in the region. Quartz veins, with typical crustiform–colloform banded structures, fill WNW, sub-vertical, normal faults, originating from extensional tectonics. The silicification of travertines, tuffs and breccia is the most common hydrothermal alteration.
publishDate 2016
dc.date.none.fl_str_mv 2016
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
Articulo
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://sedici.unlp.edu.ar/handle/10915/85857
url http://sedici.unlp.edu.ar/handle/10915/85857
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/issn/1744-5647
info:eu-repo/semantics/altIdentifier/doi/10.1080/17445647.2016.1187676
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by-nc-sa/4.0/
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)
dc.format.none.fl_str_mv application/pdf
172-177
dc.source.none.fl_str_mv reponame:SEDICI (UNLP)
instname:Universidad Nacional de La Plata
instacron:UNLP
reponame_str SEDICI (UNLP)
collection SEDICI (UNLP)
instname_str Universidad Nacional de La Plata
instacron_str UNLP
institution UNLP
repository.name.fl_str_mv SEDICI (UNLP) - Universidad Nacional de La Plata
repository.mail.fl_str_mv alira@sedici.unlp.edu.ar
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