Chemical and isotopic composition of hot spring waters in the Tacna region, Southern Peru

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16 páginas
Detalles Bibliográficos
Autor: Cruz Pauccara, Vicentina
Formato: documento de trabajo
Fecha de Publicación:2018
Institución:Instituto Geológico, Minero y Metalúrgico
Repositorio:INGEMMET-Institucional
Lenguaje:español
OAI Identifier:oai:repositorio.ingemmet.gob.pe:20.500.12544/3488
Enlace del recurso:https://hdl.handle.net/20.500.12544/3488
Nivel de acceso:acceso abierto
Materia:Aguas termales
Composición química
Isótopos
Tectónica
Recursos geotérmicos
http://purl.org/pe-repo/ocde/ford#1.05.00
http://purl.org/pe-repo/ocde/ford#1.05.06
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dc.title.es_PE.fl_str_mv Chemical and isotopic composition of hot spring waters in the Tacna region, Southern Peru
title Chemical and isotopic composition of hot spring waters in the Tacna region, Southern Peru
spellingShingle Chemical and isotopic composition of hot spring waters in the Tacna region, Southern Peru
Cruz Pauccara, Vicentina
Aguas termales
Composición química
Isótopos
Tectónica
Recursos geotérmicos
http://purl.org/pe-repo/ocde/ford#1.05.00
http://purl.org/pe-repo/ocde/ford#1.05.06
title_short Chemical and isotopic composition of hot spring waters in the Tacna region, Southern Peru
title_full Chemical and isotopic composition of hot spring waters in the Tacna region, Southern Peru
title_fullStr Chemical and isotopic composition of hot spring waters in the Tacna region, Southern Peru
title_full_unstemmed Chemical and isotopic composition of hot spring waters in the Tacna region, Southern Peru
title_sort Chemical and isotopic composition of hot spring waters in the Tacna region, Southern Peru
author Cruz Pauccara, Vicentina
author_facet Cruz Pauccara, Vicentina
author_role author
dc.contributor.author.fl_str_mv Cruz Pauccara, Vicentina
dc.subject.es_PE.fl_str_mv Aguas termales
Composición química
Isótopos
Tectónica
Recursos geotérmicos
topic Aguas termales
Composición química
Isótopos
Tectónica
Recursos geotérmicos
http://purl.org/pe-repo/ocde/ford#1.05.00
http://purl.org/pe-repo/ocde/ford#1.05.06
dc.subject.ocde.es_PE.fl_str_mv http://purl.org/pe-repo/ocde/ford#1.05.00
http://purl.org/pe-repo/ocde/ford#1.05.06
description 16 páginas
publishDate 2018
dc.date.accessioned.none.fl_str_mv 2021-11-19T15:02:47Z
dc.date.available.none.fl_str_mv 2021-11-19T15:02:47Z
dc.date.issued.fl_str_mv 2018-02
dc.type.es_PE.fl_str_mv info:eu-repo/semantics/workingPaper
dc.type.version.es_PE.fl_str_mv info:eu-repo/semantics/publishedVersion
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dc.identifier.citation.es_PE.fl_str_mv Cruz, V. (2018). Chemical and isotopic composition of hot spring waters in the Tacna region, Southern Peru. Instituto Geológico, Minero y Metalúrgico, 2018, 16 p.
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/20.500.12544/3488
identifier_str_mv Cruz, V. (2018). Chemical and isotopic composition of hot spring waters in the Tacna region, Southern Peru. Instituto Geológico, Minero y Metalúrgico, 2018, 16 p.
url https://hdl.handle.net/20.500.12544/3488
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language spa
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dc.format.es_PE.fl_str_mv application/pdf
dc.coverage.spatial.es_PE.fl_str_mv Tacna
Perú
dc.publisher.es_PE.fl_str_mv Instituto Geológico, Minero y Metalúrgico - INGEMMET
dc.publisher.country.es_PE.fl_str_mv PE
dc.source.es_PE.fl_str_mv Repositorio Institucional INGEMMET
Instituto Geológico, Minero y Metalúrgico – INGEMMET
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spelling Cruz Pauccara, VicentinaTacnaPerú2021-11-19T15:02:47Z2021-11-19T15:02:47Z2018-02Cruz, V. (2018). Chemical and isotopic composition of hot spring waters in the Tacna region, Southern Peru. Instituto Geológico, Minero y Metalúrgico, 2018, 16 p.https://hdl.handle.net/20.500.12544/348816 páginasThe Tacna region hosts the most promising geothermal zones of Southern Peru, comprising five main geothermal areas: Tutupaca, Calientes, Borateras, Ancocollo and Chungara- Kallapuma located along the Quaternary volcanic chain at a height of 4000-4400 m on the Cordillera de los Andes. In these areas, we studied the chemical and isotopic composition of thermal waters. The geochemical characterization of the thermal discharges shows, the presence of two different types of thermal spring in Tacna region Na+ -Cland Ca2+ -SO4 2- waters. The Na+ -Clsprings, controlled by magma degassing and by water-rock interaction processes. Ca2+ -SO4 2- waters are supply by shallow meteoric water heated by ascending gases and are characterized by a low pH. Chloride water is rich in B, As and SiO2, suggesting interactions of deep-originated fluids with meteoric waters at shallow depth. The relatively high boron concentrations in the geothermal waters may be due to deep circulation paths that interacted with different lithologies at depth associated to sedimentary rocks. The isotopic composition δ2H and δ18O indicates that the geothermal reservoir waters originate from a mixture of meteoric and magmatic water, with temperatures exceeding 200°C estimated by geothermometry, indicate that geothermal areas can be regarded as the most promising areas and deserve more detailed geological and geophysical investigations for determination the geothermal potential.application/pdfspaInstituto Geológico, Minero y Metalúrgico - INGEMMETPEinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-nd/4.0/deed.esRepositorio Institucional INGEMMETInstituto Geológico, Minero y Metalúrgico – INGEMMETreponame:INGEMMET-Institucionalinstname:Instituto Geológico, Minero y Metalúrgicoinstacron:INGEMMETAguas termalesComposición químicaIsótoposTectónicaRecursos geotérmicoshttp://purl.org/pe-repo/ocde/ford#1.05.00http://purl.org/pe-repo/ocde/ford#1.05.06Chemical and isotopic composition of hot spring waters in the Tacna region, Southern Peruinfo:eu-repo/semantics/workingPaperinfo:eu-repo/semantics/publishedVersionLICENSElicense.txtlicense.txttext/plain; charset=utf-81567https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/3488/2/license.txtecccc10c448afdeacc04912e07a3ed65MD52ORIGINALCruz-Chemical_and_isotopic_composition_hot_spring.pdfCruz-Chemical_and_isotopic_composition_hot_spring.pdfWorking paperapplication/pdf2307791https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/3488/3/Cruz-Chemical_and_isotopic_composition_hot_spring.pdf4d2c2a744eb9b6c1848137d823c8cf82MD53TEXTCruz-Chemical_and_isotopic_composition_hot_spring.pdf.txtCruz-Chemical_and_isotopic_composition_hot_spring.pdf.txtExtracted texttext/plain68606https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/3488/4/Cruz-Chemical_and_isotopic_composition_hot_spring.pdf.txta5346197e3ef2f53088c877fed23cdcdMD54THUMBNAILCruz-Chemical_and_isotopic_composition_hot_spring.pdf.jpgCruz-Chemical_and_isotopic_composition_hot_spring.pdf.jpgGenerated Thumbnailimage/jpeg25519https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/3488/5/Cruz-Chemical_and_isotopic_composition_hot_spring.pdf.jpgbc88f23394b9ed97ba1a3cd6cc0c83fcMD5520.500.12544/3488oai:repositorio.ingemmet.gob.pe:20.500.12544/34882021-12-13 11:53:15.88Repositorio Institucional INGEMMETrepositorio@ingemmet.gob.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