Boron isotope composition of geothermal fluids and borate minerals from salar deposits (central Andes/NW Argentina)

Autores
Kasemann, Simone A.; Meixner, Anette; Erzinger, Jörg; Viramonte, Jose German; Alonso, Ricardo Narciso; Franz, Gerhard
Año de publicación
2004
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
We have measured the boron concentration and isotope composition of regionally expansive borate deposits and geothermal fluids from the Cenozoic geothermal system of the Argentine Puna Plateau in the central Andes. The borate minerals borax, colemanite, hydroboracite, inderite, inyoite, kernite, teruggite, tincalconite, and ulexite span a wide range of d 11B values from 229.5 to 20.3‰, whereas fluids cover a range from 218.3 to 0.7‰. The data from recent coexisting borate minerals and fluids allow for the calculation of the isotope composition of the ancient mineralizing fluids and thus for the constraint of the isotope composition of the source rocks sampled by the fluids. The boron isotope composition of ancient mineralizing fluids appears uniform throughout the section of precipitates at a given locality and similar to values obtained from recent thermal fluids. These findings support models that suggest uniform and stable climatic, magmatic, and tectonic
conditions during the past 8 million years in this part of the central Andes. Boron in fluids is derived from different sources, depending on the drainage system and local country rocks. One significant boron source is the Paleozoic basement, which has a whole-rock isotopic composition of d 11B ¼ 28.9 ^ 2.2‰ (1 SD); another important boron contribution comes from Neogene-Pleistocene ignimbrites (d 11B ¼ 23.8 ^ 2.8‰, 1 SD). Cenozoic andesites and Mesozoic limestones (d 11B # þ 8‰) provide a potential third boron source.
Fil: Kasemann, Simone A.. German Research Centre for Geosciences; Alemania
Fil: Meixner, Anette. German Research Centre for Geosciences; Alemania
Fil: Erzinger, Jörg. German Research Centre for Geosciences; Alemania
Fil: Viramonte, Jose German. Universidad Nacional de Salta; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Alonso, Ricardo Narciso. Universidad Nacional de Salta; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Franz, Gerhard. Technishe Universitat Berlin; Alemania
Materia
BORATE DEPOSITS
BORON ISOTOPES
CENTRAL ANDES
GEOTHERMAL FLUIDS
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/186539

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repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Boron isotope composition of geothermal fluids and borate minerals from salar deposits (central Andes/NW Argentina)Kasemann, Simone A.Meixner, AnetteErzinger, JörgViramonte, Jose GermanAlonso, Ricardo NarcisoFranz, GerhardBORATE DEPOSITSBORON ISOTOPESCENTRAL ANDESGEOTHERMAL FLUIDShttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1We have measured the boron concentration and isotope composition of regionally expansive borate deposits and geothermal fluids from the Cenozoic geothermal system of the Argentine Puna Plateau in the central Andes. The borate minerals borax, colemanite, hydroboracite, inderite, inyoite, kernite, teruggite, tincalconite, and ulexite span a wide range of d 11B values from 229.5 to 20.3‰, whereas fluids cover a range from 218.3 to 0.7‰. The data from recent coexisting borate minerals and fluids allow for the calculation of the isotope composition of the ancient mineralizing fluids and thus for the constraint of the isotope composition of the source rocks sampled by the fluids. The boron isotope composition of ancient mineralizing fluids appears uniform throughout the section of precipitates at a given locality and similar to values obtained from recent thermal fluids. These findings support models that suggest uniform and stable climatic, magmatic, and tectonic<br />conditions during the past 8 million years in this part of the central Andes. Boron in fluids is derived from different sources, depending on the drainage system and local country rocks. One significant boron source is the Paleozoic basement, which has a whole-rock isotopic composition of d 11B ¼ 28.9 ^ 2.2‰ (1 SD); another important boron contribution comes from Neogene-Pleistocene ignimbrites (d 11B ¼ 23.8 ^ 2.8‰, 1 SD). Cenozoic andesites and Mesozoic limestones (d 11B # þ 8‰) provide a potential third boron source.Fil: Kasemann, Simone A.. German Research Centre for Geosciences; AlemaniaFil: Meixner, Anette. German Research Centre for Geosciences; AlemaniaFil: Erzinger, Jörg. German Research Centre for Geosciences; AlemaniaFil: Viramonte, Jose German. Universidad Nacional de Salta; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Alonso, Ricardo Narciso. Universidad Nacional de Salta; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Franz, Gerhard. Technishe Universitat Berlin; AlemaniaPergamon-Elsevier Science Ltd2004-06info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/186539Kasemann, Simone A.; Meixner, Anette; Erzinger, Jörg; Viramonte, Jose German; Alonso, Ricardo Narciso; et al.; Boron isotope composition of geothermal fluids and borate minerals from salar deposits (central Andes/NW Argentina); Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 16; 8; 6-2004; 685-6970895-9811CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1016/j.jsames.2003.12.004info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:30:45Zoai:ri.conicet.gov.ar:11336/186539instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 10:30:45.689CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Boron isotope composition of geothermal fluids and borate minerals from salar deposits (central Andes/NW Argentina)
title Boron isotope composition of geothermal fluids and borate minerals from salar deposits (central Andes/NW Argentina)
spellingShingle Boron isotope composition of geothermal fluids and borate minerals from salar deposits (central Andes/NW Argentina)
Kasemann, Simone A.
BORATE DEPOSITS
BORON ISOTOPES
CENTRAL ANDES
GEOTHERMAL FLUIDS
title_short Boron isotope composition of geothermal fluids and borate minerals from salar deposits (central Andes/NW Argentina)
title_full Boron isotope composition of geothermal fluids and borate minerals from salar deposits (central Andes/NW Argentina)
title_fullStr Boron isotope composition of geothermal fluids and borate minerals from salar deposits (central Andes/NW Argentina)
title_full_unstemmed Boron isotope composition of geothermal fluids and borate minerals from salar deposits (central Andes/NW Argentina)
title_sort Boron isotope composition of geothermal fluids and borate minerals from salar deposits (central Andes/NW Argentina)
dc.creator.none.fl_str_mv Kasemann, Simone A.
Meixner, Anette
Erzinger, Jörg
Viramonte, Jose German
Alonso, Ricardo Narciso
Franz, Gerhard
author Kasemann, Simone A.
author_facet Kasemann, Simone A.
Meixner, Anette
Erzinger, Jörg
Viramonte, Jose German
Alonso, Ricardo Narciso
Franz, Gerhard
author_role author
author2 Meixner, Anette
Erzinger, Jörg
Viramonte, Jose German
Alonso, Ricardo Narciso
Franz, Gerhard
author2_role author
author
author
author
author
dc.subject.none.fl_str_mv BORATE DEPOSITS
BORON ISOTOPES
CENTRAL ANDES
GEOTHERMAL FLUIDS
topic BORATE DEPOSITS
BORON ISOTOPES
CENTRAL ANDES
GEOTHERMAL FLUIDS
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv We have measured the boron concentration and isotope composition of regionally expansive borate deposits and geothermal fluids from the Cenozoic geothermal system of the Argentine Puna Plateau in the central Andes. The borate minerals borax, colemanite, hydroboracite, inderite, inyoite, kernite, teruggite, tincalconite, and ulexite span a wide range of d 11B values from 229.5 to 20.3‰, whereas fluids cover a range from 218.3 to 0.7‰. The data from recent coexisting borate minerals and fluids allow for the calculation of the isotope composition of the ancient mineralizing fluids and thus for the constraint of the isotope composition of the source rocks sampled by the fluids. The boron isotope composition of ancient mineralizing fluids appears uniform throughout the section of precipitates at a given locality and similar to values obtained from recent thermal fluids. These findings support models that suggest uniform and stable climatic, magmatic, and tectonic<br />conditions during the past 8 million years in this part of the central Andes. Boron in fluids is derived from different sources, depending on the drainage system and local country rocks. One significant boron source is the Paleozoic basement, which has a whole-rock isotopic composition of d 11B ¼ 28.9 ^ 2.2‰ (1 SD); another important boron contribution comes from Neogene-Pleistocene ignimbrites (d 11B ¼ 23.8 ^ 2.8‰, 1 SD). Cenozoic andesites and Mesozoic limestones (d 11B # þ 8‰) provide a potential third boron source.
Fil: Kasemann, Simone A.. German Research Centre for Geosciences; Alemania
Fil: Meixner, Anette. German Research Centre for Geosciences; Alemania
Fil: Erzinger, Jörg. German Research Centre for Geosciences; Alemania
Fil: Viramonte, Jose German. Universidad Nacional de Salta; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Alonso, Ricardo Narciso. Universidad Nacional de Salta; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Franz, Gerhard. Technishe Universitat Berlin; Alemania
description We have measured the boron concentration and isotope composition of regionally expansive borate deposits and geothermal fluids from the Cenozoic geothermal system of the Argentine Puna Plateau in the central Andes. The borate minerals borax, colemanite, hydroboracite, inderite, inyoite, kernite, teruggite, tincalconite, and ulexite span a wide range of d 11B values from 229.5 to 20.3‰, whereas fluids cover a range from 218.3 to 0.7‰. The data from recent coexisting borate minerals and fluids allow for the calculation of the isotope composition of the ancient mineralizing fluids and thus for the constraint of the isotope composition of the source rocks sampled by the fluids. The boron isotope composition of ancient mineralizing fluids appears uniform throughout the section of precipitates at a given locality and similar to values obtained from recent thermal fluids. These findings support models that suggest uniform and stable climatic, magmatic, and tectonic<br />conditions during the past 8 million years in this part of the central Andes. Boron in fluids is derived from different sources, depending on the drainage system and local country rocks. One significant boron source is the Paleozoic basement, which has a whole-rock isotopic composition of d 11B ¼ 28.9 ^ 2.2‰ (1 SD); another important boron contribution comes from Neogene-Pleistocene ignimbrites (d 11B ¼ 23.8 ^ 2.8‰, 1 SD). Cenozoic andesites and Mesozoic limestones (d 11B # þ 8‰) provide a potential third boron source.
publishDate 2004
dc.date.none.fl_str_mv 2004-06
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/11336/186539
Kasemann, Simone A.; Meixner, Anette; Erzinger, Jörg; Viramonte, Jose German; Alonso, Ricardo Narciso; et al.; Boron isotope composition of geothermal fluids and borate minerals from salar deposits (central Andes/NW Argentina); Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 16; 8; 6-2004; 685-697
0895-9811
CONICET Digital
CONICET
url http://hdl.handle.net/11336/186539
identifier_str_mv Kasemann, Simone A.; Meixner, Anette; Erzinger, Jörg; Viramonte, Jose German; Alonso, Ricardo Narciso; et al.; Boron isotope composition of geothermal fluids and borate minerals from salar deposits (central Andes/NW Argentina); Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 16; 8; 6-2004; 685-697
0895-9811
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jsames.2003.12.004
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
application/pdf
dc.publisher.none.fl_str_mv Pergamon-Elsevier Science Ltd
publisher.none.fl_str_mv Pergamon-Elsevier Science Ltd
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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