Analysis of a storm-flood-dominated delta succession from the Cretaceous of Patagonia (Austral-Magallanes basin)

Autores
Moyano Paz, Damián; Isla, Manuel Fermín; Mon, Lucas Francisco; Buatois, Luis Alberto; Richiano, Sebastián Miguel; Olivo, Mariana Soledad; Cutiño, José I.; Poire, Daniel Gustavo
Año de publicación
2025
Idioma
inglés
Tipo de recurso
documento de conferencia
Estado
versión publicada
Descripción
Storm-flood-dominated deltas are shaped by the interaction of river floods and storm waves, where continental and open marine processes act simultaneously during storms. Their stratigraphic record remains poorly constrained, especially regarding facies variability and ichnological features. To address this, we conducted a high-resolution sedimentological and ichnological analysis of a 75-m-thick sedimentary succession of the Piedra Clavada/Kachaike Formation (Cretaceous, AustralMagallanes Basin), to: (i) decipher the variability of depositional processes linked to storm-flood events, and (ii) assess the physicochemical conditions influencing trace-making communities. Facies associations (FAs) analysis reveals multiple deltaic-coastal elements, including complex prodelta fines, storm-flood frontal splays and channels, mouth bars, and storm-wave sandstone bodies. FAs record the interaction of hyperpycnal flows, hypopycnal plumes, wave-enhanced muddy gravity flows, and both fair-weather and storm wave processes, at both bed and bedset scales. These suggest deposition during storm-flood events alternating with inter-event (i.e., fair-weather) periods, mostly in prodelta to delta-front settings under storm-flood dominance. Vertical stacking evaluation and bounding-surface analysis allowed the recognition of 3 hierarchical levels of highresolution genetic units: (i) two parasequences separated by a transgressive surface, the lower further subdivided into (ii) bedsets bounded by flooding surfaces; and (iii) sub-bedsets bounded by minor flooding surfaces. This stratigraphic framework reveals the autogenic and allogenic controls on storm-flood delta stratigraphy and provides insights into delta-lobe evolution under event-dominated conditions. Storm-flood dynamics additionally generate complex physicochemical conditions reflected in the ichnological signatures of the deposits. The overall reduction in bioturbation intensities (BI 0–5, typically 0–1), with extended intervals lacking bioturbation suggest that elevated sedimentation rates represented a primary stress for tracemakers, with limited colonization windows. The low ichnodiversity of these deposits, in addition with the presence of syneresis cracks suggest short-lived periods of reduced salinity. The dominance of structures positively correlated to mobile and sessile deposit-feeding strategies in detriment of suspension-feeding structures, which are markedly absent, indicate elevated water turbidity. Abundant phytodetrital pulses might also favor reduced bottomwater oxygenation resulting in unburrowed beds or suites dominated by Chondrites and Trichichnus. Rapid mud deposition via gravitational collapse of buoyant plumes or tractive remobilization likely produced fluid-mud substrates (soupground), which are mostly devoid of bioturbation or show only scattered sediment-swimming structures (navichnia) or deformed traces.
Fil: Moyano Paz, Damián. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: Isla, Manuel Fermín. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: Mon, Lucas Francisco. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: Buatois, Luis Alberto. Department Geological Sciences ; University Of Saskatchewan; . Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología. Cátedra Geología Estructural. Instituto Superior de Correlación Geológica; Argentina
Fil: Richiano, Sebastián Miguel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Nacional Patagónico; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: Olivo, Mariana Soledad. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina
Fil: Cutiño, José I.. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Nacional Patagónico; Argentina
Fil: Poire, Daniel Gustavo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
XIX Reunión Argentina de Sedimentología: La Sedimentología en la era de la Ciencia de Datos
Córoba
Argentina
Asociación Argentina de Sedimentología
Materia
STORM DEPOSITS
DELTA SYSTEMS
PIEDRA CLAVADA FORMATION
CRETACEOUS
AUSTRAL-MAGALLANES BASIN
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:11336/275049
Acceder
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network_name_str CONICET Digital (CONICET)
spelling Analysis of a storm-flood-dominated delta succession from the Cretaceous of Patagonia (Austral-Magallanes basin)Moyano Paz, DamiánIsla, Manuel FermínMon, Lucas FranciscoBuatois, Luis AlbertoRichiano, Sebastián MiguelOlivo, Mariana SoledadCutiño, José I.Poire, Daniel GustavoSTORM DEPOSITSDELTA SYSTEMSPIEDRA CLAVADA FORMATIONCRETACEOUSAUSTRAL-MAGALLANES BASINhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Storm-flood-dominated deltas are shaped by the interaction of river floods and storm waves, where continental and open marine processes act simultaneously during storms. Their stratigraphic record remains poorly constrained, especially regarding facies variability and ichnological features. To address this, we conducted a high-resolution sedimentological and ichnological analysis of a 75-m-thick sedimentary succession of the Piedra Clavada/Kachaike Formation (Cretaceous, AustralMagallanes Basin), to: (i) decipher the variability of depositional processes linked to storm-flood events, and (ii) assess the physicochemical conditions influencing trace-making communities. Facies associations (FAs) analysis reveals multiple deltaic-coastal elements, including complex prodelta fines, storm-flood frontal splays and channels, mouth bars, and storm-wave sandstone bodies. FAs record the interaction of hyperpycnal flows, hypopycnal plumes, wave-enhanced muddy gravity flows, and both fair-weather and storm wave processes, at both bed and bedset scales. These suggest deposition during storm-flood events alternating with inter-event (i.e., fair-weather) periods, mostly in prodelta to delta-front settings under storm-flood dominance. Vertical stacking evaluation and bounding-surface analysis allowed the recognition of 3 hierarchical levels of highresolution genetic units: (i) two parasequences separated by a transgressive surface, the lower further subdivided into (ii) bedsets bounded by flooding surfaces; and (iii) sub-bedsets bounded by minor flooding surfaces. This stratigraphic framework reveals the autogenic and allogenic controls on storm-flood delta stratigraphy and provides insights into delta-lobe evolution under event-dominated conditions. Storm-flood dynamics additionally generate complex physicochemical conditions reflected in the ichnological signatures of the deposits. The overall reduction in bioturbation intensities (BI 0–5, typically 0–1), with extended intervals lacking bioturbation suggest that elevated sedimentation rates represented a primary stress for tracemakers, with limited colonization windows. The low ichnodiversity of these deposits, in addition with the presence of syneresis cracks suggest short-lived periods of reduced salinity. The dominance of structures positively correlated to mobile and sessile deposit-feeding strategies in detriment of suspension-feeding structures, which are markedly absent, indicate elevated water turbidity. Abundant phytodetrital pulses might also favor reduced bottomwater oxygenation resulting in unburrowed beds or suites dominated by Chondrites and Trichichnus. Rapid mud deposition via gravitational collapse of buoyant plumes or tractive remobilization likely produced fluid-mud substrates (soupground), which are mostly devoid of bioturbation or show only scattered sediment-swimming structures (navichnia) or deformed traces.Fil: Moyano Paz, Damián. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; ArgentinaFil: Isla, Manuel Fermín. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; ArgentinaFil: Mon, Lucas Francisco. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; ArgentinaFil: Buatois, Luis Alberto. Department Geological Sciences ; University Of Saskatchewan; . Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología. Cátedra Geología Estructural. Instituto Superior de Correlación Geológica; ArgentinaFil: Richiano, Sebastián Miguel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Nacional Patagónico; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; ArgentinaFil: Olivo, Mariana Soledad. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; ArgentinaFil: Cutiño, José I.. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Nacional Patagónico; ArgentinaFil: Poire, Daniel Gustavo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; ArgentinaXIX Reunión Argentina de Sedimentología: La Sedimentología en la era de la Ciencia de DatosCórobaArgentinaAsociación Argentina de SedimentologíaAsociación Argentina de Sedimentología2025info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjectCongresoBookhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/275049Analysis of a storm-flood-dominated delta succession from the Cretaceous of Patagonia (Austral-Magallanes basin); XIX Reunión Argentina de Sedimentología: La Sedimentología en la era de la Ciencia de Datos; Córoba; Argentina; 2025; 115-115978-631-90299-2-5CONICET DigitalCONICETengNacionalinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-12-03T08:39:30Zoai:ri.conicet.gov.ar:11336/275049instacron: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:34982025-12-03 08:39:31.11CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Analysis of a storm-flood-dominated delta succession from the Cretaceous of Patagonia (Austral-Magallanes basin)
title Analysis of a storm-flood-dominated delta succession from the Cretaceous of Patagonia (Austral-Magallanes basin)
spellingShingle Analysis of a storm-flood-dominated delta succession from the Cretaceous of Patagonia (Austral-Magallanes basin)
Moyano Paz, Damián
STORM DEPOSITS
DELTA SYSTEMS
PIEDRA CLAVADA FORMATION
CRETACEOUS
AUSTRAL-MAGALLANES BASIN
title_short Analysis of a storm-flood-dominated delta succession from the Cretaceous of Patagonia (Austral-Magallanes basin)
title_full Analysis of a storm-flood-dominated delta succession from the Cretaceous of Patagonia (Austral-Magallanes basin)
title_fullStr Analysis of a storm-flood-dominated delta succession from the Cretaceous of Patagonia (Austral-Magallanes basin)
title_full_unstemmed Analysis of a storm-flood-dominated delta succession from the Cretaceous of Patagonia (Austral-Magallanes basin)
title_sort Analysis of a storm-flood-dominated delta succession from the Cretaceous of Patagonia (Austral-Magallanes basin)
dc.creator.none.fl_str_mv Moyano Paz, Damián
Isla, Manuel Fermín
Mon, Lucas Francisco
Buatois, Luis Alberto
Richiano, Sebastián Miguel
Olivo, Mariana Soledad
Cutiño, José I.
Poire, Daniel Gustavo
author Moyano Paz, Damián
author_facet Moyano Paz, Damián
Isla, Manuel Fermín
Mon, Lucas Francisco
Buatois, Luis Alberto
Richiano, Sebastián Miguel
Olivo, Mariana Soledad
Cutiño, José I.
Poire, Daniel Gustavo
author_role author
author2 Isla, Manuel Fermín
Mon, Lucas Francisco
Buatois, Luis Alberto
Richiano, Sebastián Miguel
Olivo, Mariana Soledad
Cutiño, José I.
Poire, Daniel Gustavo
author2_role author
author
author
author
author
author
author
dc.subject.none.fl_str_mv STORM DEPOSITS
DELTA SYSTEMS
PIEDRA CLAVADA FORMATION
CRETACEOUS
AUSTRAL-MAGALLANES BASIN
topic STORM DEPOSITS
DELTA SYSTEMS
PIEDRA CLAVADA FORMATION
CRETACEOUS
AUSTRAL-MAGALLANES BASIN
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Storm-flood-dominated deltas are shaped by the interaction of river floods and storm waves, where continental and open marine processes act simultaneously during storms. Their stratigraphic record remains poorly constrained, especially regarding facies variability and ichnological features. To address this, we conducted a high-resolution sedimentological and ichnological analysis of a 75-m-thick sedimentary succession of the Piedra Clavada/Kachaike Formation (Cretaceous, AustralMagallanes Basin), to: (i) decipher the variability of depositional processes linked to storm-flood events, and (ii) assess the physicochemical conditions influencing trace-making communities. Facies associations (FAs) analysis reveals multiple deltaic-coastal elements, including complex prodelta fines, storm-flood frontal splays and channels, mouth bars, and storm-wave sandstone bodies. FAs record the interaction of hyperpycnal flows, hypopycnal plumes, wave-enhanced muddy gravity flows, and both fair-weather and storm wave processes, at both bed and bedset scales. These suggest deposition during storm-flood events alternating with inter-event (i.e., fair-weather) periods, mostly in prodelta to delta-front settings under storm-flood dominance. Vertical stacking evaluation and bounding-surface analysis allowed the recognition of 3 hierarchical levels of highresolution genetic units: (i) two parasequences separated by a transgressive surface, the lower further subdivided into (ii) bedsets bounded by flooding surfaces; and (iii) sub-bedsets bounded by minor flooding surfaces. This stratigraphic framework reveals the autogenic and allogenic controls on storm-flood delta stratigraphy and provides insights into delta-lobe evolution under event-dominated conditions. Storm-flood dynamics additionally generate complex physicochemical conditions reflected in the ichnological signatures of the deposits. The overall reduction in bioturbation intensities (BI 0–5, typically 0–1), with extended intervals lacking bioturbation suggest that elevated sedimentation rates represented a primary stress for tracemakers, with limited colonization windows. The low ichnodiversity of these deposits, in addition with the presence of syneresis cracks suggest short-lived periods of reduced salinity. The dominance of structures positively correlated to mobile and sessile deposit-feeding strategies in detriment of suspension-feeding structures, which are markedly absent, indicate elevated water turbidity. Abundant phytodetrital pulses might also favor reduced bottomwater oxygenation resulting in unburrowed beds or suites dominated by Chondrites and Trichichnus. Rapid mud deposition via gravitational collapse of buoyant plumes or tractive remobilization likely produced fluid-mud substrates (soupground), which are mostly devoid of bioturbation or show only scattered sediment-swimming structures (navichnia) or deformed traces.
Fil: Moyano Paz, Damián. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: Isla, Manuel Fermín. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: Mon, Lucas Francisco. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: Buatois, Luis Alberto. Department Geological Sciences ; University Of Saskatchewan; . Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología. Cátedra Geología Estructural. Instituto Superior de Correlación Geológica; Argentina
Fil: Richiano, Sebastián Miguel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Nacional Patagónico; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: Olivo, Mariana Soledad. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina
Fil: Cutiño, José I.. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Nacional Patagónico; Argentina
Fil: Poire, Daniel Gustavo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
XIX Reunión Argentina de Sedimentología: La Sedimentología en la era de la Ciencia de Datos
Córoba
Argentina
Asociación Argentina de Sedimentología
description Storm-flood-dominated deltas are shaped by the interaction of river floods and storm waves, where continental and open marine processes act simultaneously during storms. Their stratigraphic record remains poorly constrained, especially regarding facies variability and ichnological features. To address this, we conducted a high-resolution sedimentological and ichnological analysis of a 75-m-thick sedimentary succession of the Piedra Clavada/Kachaike Formation (Cretaceous, AustralMagallanes Basin), to: (i) decipher the variability of depositional processes linked to storm-flood events, and (ii) assess the physicochemical conditions influencing trace-making communities. Facies associations (FAs) analysis reveals multiple deltaic-coastal elements, including complex prodelta fines, storm-flood frontal splays and channels, mouth bars, and storm-wave sandstone bodies. FAs record the interaction of hyperpycnal flows, hypopycnal plumes, wave-enhanced muddy gravity flows, and both fair-weather and storm wave processes, at both bed and bedset scales. These suggest deposition during storm-flood events alternating with inter-event (i.e., fair-weather) periods, mostly in prodelta to delta-front settings under storm-flood dominance. Vertical stacking evaluation and bounding-surface analysis allowed the recognition of 3 hierarchical levels of highresolution genetic units: (i) two parasequences separated by a transgressive surface, the lower further subdivided into (ii) bedsets bounded by flooding surfaces; and (iii) sub-bedsets bounded by minor flooding surfaces. This stratigraphic framework reveals the autogenic and allogenic controls on storm-flood delta stratigraphy and provides insights into delta-lobe evolution under event-dominated conditions. Storm-flood dynamics additionally generate complex physicochemical conditions reflected in the ichnological signatures of the deposits. The overall reduction in bioturbation intensities (BI 0–5, typically 0–1), with extended intervals lacking bioturbation suggest that elevated sedimentation rates represented a primary stress for tracemakers, with limited colonization windows. The low ichnodiversity of these deposits, in addition with the presence of syneresis cracks suggest short-lived periods of reduced salinity. The dominance of structures positively correlated to mobile and sessile deposit-feeding strategies in detriment of suspension-feeding structures, which are markedly absent, indicate elevated water turbidity. Abundant phytodetrital pulses might also favor reduced bottomwater oxygenation resulting in unburrowed beds or suites dominated by Chondrites and Trichichnus. Rapid mud deposition via gravitational collapse of buoyant plumes or tractive remobilization likely produced fluid-mud substrates (soupground), which are mostly devoid of bioturbation or show only scattered sediment-swimming structures (navichnia) or deformed traces.
publishDate 2025
dc.date.none.fl_str_mv 2025
dc.type.none.fl_str_mv info:eu-repo/semantics/publishedVersion
info:eu-repo/semantics/conferenceObject
Congreso
Book
http://purl.org/coar/resource_type/c_5794
info:ar-repo/semantics/documentoDeConferencia
status_str publishedVersion
format conferenceObject
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/275049
Analysis of a storm-flood-dominated delta succession from the Cretaceous of Patagonia (Austral-Magallanes basin); XIX Reunión Argentina de Sedimentología: La Sedimentología en la era de la Ciencia de Datos; Córoba; Argentina; 2025; 115-115
978-631-90299-2-5
CONICET Digital
CONICET
url http://hdl.handle.net/11336/275049
identifier_str_mv Analysis of a storm-flood-dominated delta succession from the Cretaceous of Patagonia (Austral-Magallanes basin); XIX Reunión Argentina de Sedimentología: La Sedimentología en la era de la Ciencia de Datos; Córoba; Argentina; 2025; 115-115
978-631-90299-2-5
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
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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.coverage.none.fl_str_mv Nacional
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)
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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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