Recent disturbance events recorded in the sedimentary infill of Lago Guillelmo (Argentina): tephra falls and hydrogeomorphic processes

Autores
Amat, Pablo; Villarosa, Gustavo; Beigt, Debora; Outes, Ana Valeria; Cottet, Julieta; Domínguez, Lucía Inés; Cottescu Szeraws, Alexander Nicolas Christian; Barbosa Hetherington, Andrés
Año de publicación
2023
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
We studied two natural disturbances that affect the Parque Nacional NahuelHuapi area: tephra fall events from Andean volcanoes and hydrogeomorphicprocesses within catchments related to heavy rains. We carried out a surfaceanalysis, describing the main morphometric features of the selected watershed,informally called La Cantera watershed; analyzing satellite images and historicalaerial photographs; looking for evidence of processes related to these disturbanceevents in the watershed and morphological changes in the alluvial fan generatedover the delta. The subaqueous environment was analyzed through bathymetries,sediment cores, and Ground Penetrating Radar (GPR) profiles, taken in the distaldeltaic environment of the watershed. In the sedimentary record of the lake, weidentified 12 tephra layers deposited in the last 200 years, attributed to CordónCaulle, Calbuco, and Osorno volcanoes. These were chronologically correlatedwith previously documented eruptions of these volcanic centers, using vitroclastmorphology, mineral association, and stratigraphic position. We also identified10 epiclastic layers corresponding to sediments with terrigenous componentsand terrestrial organic matter, interpreted as hyperpycnites. We assign twohyperpycnite deposits to a debris flow that occurred in the area in February 2015that caused several damages and roadblocks, based on the stratigraphic positionof these deposits in the cores, and the identification of sediments associated withthis event on the lake surface in satellite images. After the correlation betweenthe GPR radargram units with the lacustrine cores, we associated one major radarunit with a (1) tephra layer and (2) lobe-shaped morphologies, interpreted asa hyperpycnite deposits, located in front of the outflow of an abandoned rivercourse. The results allow inferring a significant anthropic impact in the lacustrinerecord, as a result of the construction of Route 40 and gravel mining activitiesafter 1969 that affected the distal drainage network of the La Cantera watershed,generating topographic lows that make it difficult for subaerial flows to reachthe lake. This work shows the importance of the integration between subaerialprocesses that occur throughout a basin with the underwater processes that takeplace in the deltaic environment, to understand the extension and characteristicsof these natural disturbances.
Fil: Amat, Pablo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; Argentina
Fil: Villarosa, Gustavo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; Argentina
Fil: Beigt, Debora. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; Argentina
Fil: Outes, Ana Valeria. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; Argentina
Fil: Cottet, Julieta. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; Argentina
Fil: Domínguez, Lucía Inés. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; Argentina
Fil: Cottescu Szeraws, Alexander Nicolas Christian. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; Argentina
Fil: Barbosa Hetherington, Andrés. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; Argentina
Materia
DISTURBANCES
LAGO GUILLELMO
LACUSTRINE SEDIMENTATION
TEPHRAS
HYPERPYCNITES
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/240283
Acceder
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network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Recent disturbance events recorded in the sedimentary infill of Lago Guillelmo (Argentina): tephra falls and hydrogeomorphic processesAmat, PabloVillarosa, GustavoBeigt, DeboraOutes, Ana ValeriaCottet, JulietaDomínguez, Lucía InésCottescu Szeraws, Alexander Nicolas ChristianBarbosa Hetherington, AndrésDISTURBANCESLAGO GUILLELMOLACUSTRINE SEDIMENTATIONTEPHRASHYPERPYCNITEShttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1We studied two natural disturbances that affect the Parque Nacional NahuelHuapi area: tephra fall events from Andean volcanoes and hydrogeomorphicprocesses within catchments related to heavy rains. We carried out a surfaceanalysis, describing the main morphometric features of the selected watershed,informally called La Cantera watershed; analyzing satellite images and historicalaerial photographs; looking for evidence of processes related to these disturbanceevents in the watershed and morphological changes in the alluvial fan generatedover the delta. The subaqueous environment was analyzed through bathymetries,sediment cores, and Ground Penetrating Radar (GPR) profiles, taken in the distaldeltaic environment of the watershed. In the sedimentary record of the lake, weidentified 12 tephra layers deposited in the last 200 years, attributed to CordónCaulle, Calbuco, and Osorno volcanoes. These were chronologically correlatedwith previously documented eruptions of these volcanic centers, using vitroclastmorphology, mineral association, and stratigraphic position. We also identified10 epiclastic layers corresponding to sediments with terrigenous componentsand terrestrial organic matter, interpreted as hyperpycnites. We assign twohyperpycnite deposits to a debris flow that occurred in the area in February 2015that caused several damages and roadblocks, based on the stratigraphic positionof these deposits in the cores, and the identification of sediments associated withthis event on the lake surface in satellite images. After the correlation betweenthe GPR radargram units with the lacustrine cores, we associated one major radarunit with a (1) tephra layer and (2) lobe-shaped morphologies, interpreted asa hyperpycnite deposits, located in front of the outflow of an abandoned rivercourse. The results allow inferring a significant anthropic impact in the lacustrinerecord, as a result of the construction of Route 40 and gravel mining activitiesafter 1969 that affected the distal drainage network of the La Cantera watershed,generating topographic lows that make it difficult for subaerial flows to reachthe lake. This work shows the importance of the integration between subaerialprocesses that occur throughout a basin with the underwater processes that takeplace in the deltaic environment, to understand the extension and characteristicsof these natural disturbances.Fil: Amat, Pablo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; ArgentinaFil: Villarosa, Gustavo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; ArgentinaFil: Beigt, Debora. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; ArgentinaFil: Outes, Ana Valeria. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; ArgentinaFil: Cottet, Julieta. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; ArgentinaFil: Domínguez, Lucía Inés. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; ArgentinaFil: Cottescu Szeraws, Alexander Nicolas Christian. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; ArgentinaFil: Barbosa Hetherington, Andrés. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; ArgentinaAsociación Argentina de Sedimentología2023-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/240283Amat, Pablo; Villarosa, Gustavo; Beigt, Debora; Outes, Ana Valeria; Cottet, Julieta; et al.; Recent disturbance events recorded in the sedimentary infill of Lago Guillelmo (Argentina): tephra falls and hydrogeomorphic processes; Asociación Argentina de Sedimentología; Latin American Journal of Sedimentology and Basin Analysis; 30; 2; 12-2023; 163-1841669-73161851-4979CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://lajsba.sedimentologia.org.ar/index.php/lajsba/article/view/233info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T09:57:49Zoai:ri.conicet.gov.ar:11336/240283instacron: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:34982025-09-03 09:57:50.09CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Recent disturbance events recorded in the sedimentary infill of Lago Guillelmo (Argentina): tephra falls and hydrogeomorphic processes
title Recent disturbance events recorded in the sedimentary infill of Lago Guillelmo (Argentina): tephra falls and hydrogeomorphic processes
spellingShingle Recent disturbance events recorded in the sedimentary infill of Lago Guillelmo (Argentina): tephra falls and hydrogeomorphic processes
Amat, Pablo
DISTURBANCES
LAGO GUILLELMO
LACUSTRINE SEDIMENTATION
TEPHRAS
HYPERPYCNITES
title_short Recent disturbance events recorded in the sedimentary infill of Lago Guillelmo (Argentina): tephra falls and hydrogeomorphic processes
title_full Recent disturbance events recorded in the sedimentary infill of Lago Guillelmo (Argentina): tephra falls and hydrogeomorphic processes
title_fullStr Recent disturbance events recorded in the sedimentary infill of Lago Guillelmo (Argentina): tephra falls and hydrogeomorphic processes
title_full_unstemmed Recent disturbance events recorded in the sedimentary infill of Lago Guillelmo (Argentina): tephra falls and hydrogeomorphic processes
title_sort Recent disturbance events recorded in the sedimentary infill of Lago Guillelmo (Argentina): tephra falls and hydrogeomorphic processes
dc.creator.none.fl_str_mv Amat, Pablo
Villarosa, Gustavo
Beigt, Debora
Outes, Ana Valeria
Cottet, Julieta
Domínguez, Lucía Inés
Cottescu Szeraws, Alexander Nicolas Christian
Barbosa Hetherington, Andrés
author Amat, Pablo
author_facet Amat, Pablo
Villarosa, Gustavo
Beigt, Debora
Outes, Ana Valeria
Cottet, Julieta
Domínguez, Lucía Inés
Cottescu Szeraws, Alexander Nicolas Christian
Barbosa Hetherington, Andrés
author_role author
author2 Villarosa, Gustavo
Beigt, Debora
Outes, Ana Valeria
Cottet, Julieta
Domínguez, Lucía Inés
Cottescu Szeraws, Alexander Nicolas Christian
Barbosa Hetherington, Andrés
author2_role author
author
author
author
author
author
author
dc.subject.none.fl_str_mv DISTURBANCES
LAGO GUILLELMO
LACUSTRINE SEDIMENTATION
TEPHRAS
HYPERPYCNITES
topic DISTURBANCES
LAGO GUILLELMO
LACUSTRINE SEDIMENTATION
TEPHRAS
HYPERPYCNITES
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 studied two natural disturbances that affect the Parque Nacional NahuelHuapi area: tephra fall events from Andean volcanoes and hydrogeomorphicprocesses within catchments related to heavy rains. We carried out a surfaceanalysis, describing the main morphometric features of the selected watershed,informally called La Cantera watershed; analyzing satellite images and historicalaerial photographs; looking for evidence of processes related to these disturbanceevents in the watershed and morphological changes in the alluvial fan generatedover the delta. The subaqueous environment was analyzed through bathymetries,sediment cores, and Ground Penetrating Radar (GPR) profiles, taken in the distaldeltaic environment of the watershed. In the sedimentary record of the lake, weidentified 12 tephra layers deposited in the last 200 years, attributed to CordónCaulle, Calbuco, and Osorno volcanoes. These were chronologically correlatedwith previously documented eruptions of these volcanic centers, using vitroclastmorphology, mineral association, and stratigraphic position. We also identified10 epiclastic layers corresponding to sediments with terrigenous componentsand terrestrial organic matter, interpreted as hyperpycnites. We assign twohyperpycnite deposits to a debris flow that occurred in the area in February 2015that caused several damages and roadblocks, based on the stratigraphic positionof these deposits in the cores, and the identification of sediments associated withthis event on the lake surface in satellite images. After the correlation betweenthe GPR radargram units with the lacustrine cores, we associated one major radarunit with a (1) tephra layer and (2) lobe-shaped morphologies, interpreted asa hyperpycnite deposits, located in front of the outflow of an abandoned rivercourse. The results allow inferring a significant anthropic impact in the lacustrinerecord, as a result of the construction of Route 40 and gravel mining activitiesafter 1969 that affected the distal drainage network of the La Cantera watershed,generating topographic lows that make it difficult for subaerial flows to reachthe lake. This work shows the importance of the integration between subaerialprocesses that occur throughout a basin with the underwater processes that takeplace in the deltaic environment, to understand the extension and characteristicsof these natural disturbances.
Fil: Amat, Pablo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; Argentina
Fil: Villarosa, Gustavo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; Argentina
Fil: Beigt, Debora. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; Argentina
Fil: Outes, Ana Valeria. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; Argentina
Fil: Cottet, Julieta. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; Argentina
Fil: Domínguez, Lucía Inés. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; Argentina
Fil: Cottescu Szeraws, Alexander Nicolas Christian. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; Argentina
Fil: Barbosa Hetherington, Andrés. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales. Universidad Nacional del Comahue. Instituto Andino Patagónico de Tecnologías Biológicas y Geoambientales; Argentina
description We studied two natural disturbances that affect the Parque Nacional NahuelHuapi area: tephra fall events from Andean volcanoes and hydrogeomorphicprocesses within catchments related to heavy rains. We carried out a surfaceanalysis, describing the main morphometric features of the selected watershed,informally called La Cantera watershed; analyzing satellite images and historicalaerial photographs; looking for evidence of processes related to these disturbanceevents in the watershed and morphological changes in the alluvial fan generatedover the delta. The subaqueous environment was analyzed through bathymetries,sediment cores, and Ground Penetrating Radar (GPR) profiles, taken in the distaldeltaic environment of the watershed. In the sedimentary record of the lake, weidentified 12 tephra layers deposited in the last 200 years, attributed to CordónCaulle, Calbuco, and Osorno volcanoes. These were chronologically correlatedwith previously documented eruptions of these volcanic centers, using vitroclastmorphology, mineral association, and stratigraphic position. We also identified10 epiclastic layers corresponding to sediments with terrigenous componentsand terrestrial organic matter, interpreted as hyperpycnites. We assign twohyperpycnite deposits to a debris flow that occurred in the area in February 2015that caused several damages and roadblocks, based on the stratigraphic positionof these deposits in the cores, and the identification of sediments associated withthis event on the lake surface in satellite images. After the correlation betweenthe GPR radargram units with the lacustrine cores, we associated one major radarunit with a (1) tephra layer and (2) lobe-shaped morphologies, interpreted asa hyperpycnite deposits, located in front of the outflow of an abandoned rivercourse. The results allow inferring a significant anthropic impact in the lacustrinerecord, as a result of the construction of Route 40 and gravel mining activitiesafter 1969 that affected the distal drainage network of the La Cantera watershed,generating topographic lows that make it difficult for subaerial flows to reachthe lake. This work shows the importance of the integration between subaerialprocesses that occur throughout a basin with the underwater processes that takeplace in the deltaic environment, to understand the extension and characteristicsof these natural disturbances.
publishDate 2023
dc.date.none.fl_str_mv 2023-12
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/11336/240283
Amat, Pablo; Villarosa, Gustavo; Beigt, Debora; Outes, Ana Valeria; Cottet, Julieta; et al.; Recent disturbance events recorded in the sedimentary infill of Lago Guillelmo (Argentina): tephra falls and hydrogeomorphic processes; Asociación Argentina de Sedimentología; Latin American Journal of Sedimentology and Basin Analysis; 30; 2; 12-2023; 163-184
1669-7316
1851-4979
CONICET Digital
CONICET
url http://hdl.handle.net/11336/240283
identifier_str_mv Amat, Pablo; Villarosa, Gustavo; Beigt, Debora; Outes, Ana Valeria; Cottet, Julieta; et al.; Recent disturbance events recorded in the sedimentary infill of Lago Guillelmo (Argentina): tephra falls and hydrogeomorphic processes; Asociación Argentina de Sedimentología; Latin American Journal of Sedimentology and Basin Analysis; 30; 2; 12-2023; 163-184
1669-7316
1851-4979
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://lajsba.sedimentologia.org.ar/index.php/lajsba/article/view/233
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Asociación Argentina de Sedimentología
publisher.none.fl_str_mv Asociación Argentina de Sedimentología
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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score 13.13397

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