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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/186539
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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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1844614316300435456 |
score |
13.070432 |