The Chubut Group (Cretaceous, Golfo San Jorge Basin): A synthesis of its sedimentary petrography
- Autores
- Olazábal, Sabrina Ximena; Tunik, Maisa Andrea; Paredes, José Matildo; Allard, Jose Oscar; Foix, Nicolas
- Año de publicación
- 2025
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- This study presents a synthesis of petrographic analyses of the cretaceous Pozo D-129, Matasiete, Castillo, and Bajo Barreal formations in the Golfo San Jorge Basin, highlighting the influence of volcanic activity and sediment supply on the evolution of the Chubut Group. Data from outcrops in the San Bernardo Fold Belt and from the subsurface indicate that sandstone compositional variability was controlled by shifts in sediment source areas, linked to regional tectonic processes and active volcanism. Sandstones exhibit feldspatho-lithic and litho-feldspathic qFL, fQL, IQF to qLF composition detrital modes, with spatial and temporal variations in volcanic, pyroclastic lithic, feldspar and quartz components. The sediment sources for the outcrops in the San Bernardo Fold Belt include the Paleozoic igneous-metamorphic basement, Middle-Upper Jurassic volcanic and volcaniclastic rocks (Lonco Trapial Group), and acidic and pyroclastic sequences assigned to the Marifil Group. In contrast, the South Flank records a broader range of petrofacies, reflecting a combination of distal and local sources. In addition to the provenance of the Andes Cordillera, this sector received sediment contributions from Jurassic rocks exposed in the Deseado Region and older crystalline basement units. Andean volcanism dominates across all units, contributing direct volcanic ash fallout and reworked pyroclastic material.
Fil: Olazábal, Sabrina Ximena. Universidad Nacional de la Patagonia "San Juan Bosco". Facultad de Ciencias Naturales - Sede Comodoro. Departamento de Geología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Tunik, Maisa Andrea. Universidad Nacional de Río Negro; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Paredes, José Matildo. Universidad Nacional de la Patagonia "San Juan Bosco". Facultad de Ciencias Naturales - Sede Comodoro. Departamento de Geología; Argentina
Fil: Allard, Jose Oscar. Universidad Nacional de la Patagonia "San Juan Bosco". Facultad de Ciencias Naturales - Sede Comodoro. Departamento de Geología; Argentina
Fil: Foix, Nicolas. Universidad Nacional de la Patagonia "San Juan Bosco". Facultad de Ciencias Naturales - Sede Comodoro. Departamento de Geología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Universidad Nacional de la Patagonia San Juan Bosco. Instituto Multidisciplinario para la Investigación y el Desarrollo Productivo y Social de la Cuenca Golfo San Jorge; - Materia
-
DETRITAL MODES
VOLCANICLASTIC INPUT
SEDIMENT ROUTING
PROVENANCE
MULTIPLE SOURCE AREAS - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
.jpg)
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/291534
Ver los metadatos del registro completo
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The Chubut Group (Cretaceous, Golfo San Jorge Basin): A synthesis of its sedimentary petrographyOlazábal, Sabrina XimenaTunik, Maisa AndreaParedes, José MatildoAllard, Jose OscarFoix, NicolasDETRITAL MODESVOLCANICLASTIC INPUTSEDIMENT ROUTINGPROVENANCEMULTIPLE SOURCE AREAShttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1This study presents a synthesis of petrographic analyses of the cretaceous Pozo D-129, Matasiete, Castillo, and Bajo Barreal formations in the Golfo San Jorge Basin, highlighting the influence of volcanic activity and sediment supply on the evolution of the Chubut Group. Data from outcrops in the San Bernardo Fold Belt and from the subsurface indicate that sandstone compositional variability was controlled by shifts in sediment source areas, linked to regional tectonic processes and active volcanism. Sandstones exhibit feldspatho-lithic and litho-feldspathic qFL, fQL, IQF to qLF composition detrital modes, with spatial and temporal variations in volcanic, pyroclastic lithic, feldspar and quartz components. The sediment sources for the outcrops in the San Bernardo Fold Belt include the Paleozoic igneous-metamorphic basement, Middle-Upper Jurassic volcanic and volcaniclastic rocks (Lonco Trapial Group), and acidic and pyroclastic sequences assigned to the Marifil Group. In contrast, the South Flank records a broader range of petrofacies, reflecting a combination of distal and local sources. In addition to the provenance of the Andes Cordillera, this sector received sediment contributions from Jurassic rocks exposed in the Deseado Region and older crystalline basement units. Andean volcanism dominates across all units, contributing direct volcanic ash fallout and reworked pyroclastic material.Fil: Olazábal, Sabrina Ximena. Universidad Nacional de la Patagonia "San Juan Bosco". Facultad de Ciencias Naturales - Sede Comodoro. Departamento de Geología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Tunik, Maisa Andrea. Universidad Nacional de Río Negro; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Paredes, José Matildo. Universidad Nacional de la Patagonia "San Juan Bosco". Facultad de Ciencias Naturales - Sede Comodoro. Departamento de Geología; ArgentinaFil: Allard, Jose Oscar. Universidad Nacional de la Patagonia "San Juan Bosco". Facultad de Ciencias Naturales - Sede Comodoro. Departamento de Geología; ArgentinaFil: Foix, Nicolas. Universidad Nacional de la Patagonia "San Juan Bosco". Facultad de Ciencias Naturales - Sede Comodoro. Departamento de Geología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Universidad Nacional de la Patagonia San Juan Bosco. Instituto Multidisciplinario para la Investigación y el Desarrollo Productivo y Social de la Cuenca Golfo San Jorge;Asociación Argentina de Sedimentología2025-07info: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/11336/291534Olazábal, Sabrina Ximena; Tunik, Maisa Andrea; Paredes, José Matildo; Allard, Jose Oscar; Foix, Nicolas; The Chubut Group (Cretaceous, Golfo San Jorge Basin): A synthesis of its sedimentary petrography; Asociación Argentina de Sedimentología; Latin American Journal of Sedimentology and Basin Analysis; 32; 1; 7-2025; 44-561851-4979CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://lajsba.sedimentologia.org.ar/lajsba/article/view/277info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2026-08-25T15:05:05Zoai:ri.conicet.gov.ar:11336/291534instacron: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:34982026-08-25 15:05:06.212CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
| dc.title.none.fl_str_mv |
The Chubut Group (Cretaceous, Golfo San Jorge Basin): A synthesis of its sedimentary petrography |
| title |
The Chubut Group (Cretaceous, Golfo San Jorge Basin): A synthesis of its sedimentary petrography |
| spellingShingle |
The Chubut Group (Cretaceous, Golfo San Jorge Basin): A synthesis of its sedimentary petrography Olazábal, Sabrina Ximena DETRITAL MODES VOLCANICLASTIC INPUT SEDIMENT ROUTING PROVENANCE MULTIPLE SOURCE AREAS |
| title_short |
The Chubut Group (Cretaceous, Golfo San Jorge Basin): A synthesis of its sedimentary petrography |
| title_full |
The Chubut Group (Cretaceous, Golfo San Jorge Basin): A synthesis of its sedimentary petrography |
| title_fullStr |
The Chubut Group (Cretaceous, Golfo San Jorge Basin): A synthesis of its sedimentary petrography |
| title_full_unstemmed |
The Chubut Group (Cretaceous, Golfo San Jorge Basin): A synthesis of its sedimentary petrography |
| title_sort |
The Chubut Group (Cretaceous, Golfo San Jorge Basin): A synthesis of its sedimentary petrography |
| dc.creator.none.fl_str_mv |
Olazábal, Sabrina Ximena Tunik, Maisa Andrea Paredes, José Matildo Allard, Jose Oscar Foix, Nicolas |
| author |
Olazábal, Sabrina Ximena |
| author_facet |
Olazábal, Sabrina Ximena Tunik, Maisa Andrea Paredes, José Matildo Allard, Jose Oscar Foix, Nicolas |
| author_role |
author |
| author2 |
Tunik, Maisa Andrea Paredes, José Matildo Allard, Jose Oscar Foix, Nicolas |
| author2_role |
author author author author |
| dc.subject.none.fl_str_mv |
DETRITAL MODES VOLCANICLASTIC INPUT SEDIMENT ROUTING PROVENANCE MULTIPLE SOURCE AREAS |
| topic |
DETRITAL MODES VOLCANICLASTIC INPUT SEDIMENT ROUTING PROVENANCE MULTIPLE SOURCE AREAS |
| purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
| dc.description.none.fl_txt_mv |
This study presents a synthesis of petrographic analyses of the cretaceous Pozo D-129, Matasiete, Castillo, and Bajo Barreal formations in the Golfo San Jorge Basin, highlighting the influence of volcanic activity and sediment supply on the evolution of the Chubut Group. Data from outcrops in the San Bernardo Fold Belt and from the subsurface indicate that sandstone compositional variability was controlled by shifts in sediment source areas, linked to regional tectonic processes and active volcanism. Sandstones exhibit feldspatho-lithic and litho-feldspathic qFL, fQL, IQF to qLF composition detrital modes, with spatial and temporal variations in volcanic, pyroclastic lithic, feldspar and quartz components. The sediment sources for the outcrops in the San Bernardo Fold Belt include the Paleozoic igneous-metamorphic basement, Middle-Upper Jurassic volcanic and volcaniclastic rocks (Lonco Trapial Group), and acidic and pyroclastic sequences assigned to the Marifil Group. In contrast, the South Flank records a broader range of petrofacies, reflecting a combination of distal and local sources. In addition to the provenance of the Andes Cordillera, this sector received sediment contributions from Jurassic rocks exposed in the Deseado Region and older crystalline basement units. Andean volcanism dominates across all units, contributing direct volcanic ash fallout and reworked pyroclastic material. Fil: Olazábal, Sabrina Ximena. Universidad Nacional de la Patagonia "San Juan Bosco". Facultad de Ciencias Naturales - Sede Comodoro. Departamento de Geología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Tunik, Maisa Andrea. Universidad Nacional de Río Negro; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Paredes, José Matildo. Universidad Nacional de la Patagonia "San Juan Bosco". Facultad de Ciencias Naturales - Sede Comodoro. Departamento de Geología; Argentina Fil: Allard, Jose Oscar. Universidad Nacional de la Patagonia "San Juan Bosco". Facultad de Ciencias Naturales - Sede Comodoro. Departamento de Geología; Argentina Fil: Foix, Nicolas. Universidad Nacional de la Patagonia "San Juan Bosco". Facultad de Ciencias Naturales - Sede Comodoro. Departamento de Geología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Universidad Nacional de la Patagonia San Juan Bosco. Instituto Multidisciplinario para la Investigación y el Desarrollo Productivo y Social de la Cuenca Golfo San Jorge; |
| description |
This study presents a synthesis of petrographic analyses of the cretaceous Pozo D-129, Matasiete, Castillo, and Bajo Barreal formations in the Golfo San Jorge Basin, highlighting the influence of volcanic activity and sediment supply on the evolution of the Chubut Group. Data from outcrops in the San Bernardo Fold Belt and from the subsurface indicate that sandstone compositional variability was controlled by shifts in sediment source areas, linked to regional tectonic processes and active volcanism. Sandstones exhibit feldspatho-lithic and litho-feldspathic qFL, fQL, IQF to qLF composition detrital modes, with spatial and temporal variations in volcanic, pyroclastic lithic, feldspar and quartz components. The sediment sources for the outcrops in the San Bernardo Fold Belt include the Paleozoic igneous-metamorphic basement, Middle-Upper Jurassic volcanic and volcaniclastic rocks (Lonco Trapial Group), and acidic and pyroclastic sequences assigned to the Marifil Group. In contrast, the South Flank records a broader range of petrofacies, reflecting a combination of distal and local sources. In addition to the provenance of the Andes Cordillera, this sector received sediment contributions from Jurassic rocks exposed in the Deseado Region and older crystalline basement units. Andean volcanism dominates across all units, contributing direct volcanic ash fallout and reworked pyroclastic material. |
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2025 |
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2025-07 |
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info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
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article |
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publishedVersion |
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http://hdl.handle.net/11336/291534 Olazábal, Sabrina Ximena; Tunik, Maisa Andrea; Paredes, José Matildo; Allard, Jose Oscar; Foix, Nicolas; The Chubut Group (Cretaceous, Golfo San Jorge Basin): A synthesis of its sedimentary petrography; Asociación Argentina de Sedimentología; Latin American Journal of Sedimentology and Basin Analysis; 32; 1; 7-2025; 44-56 1851-4979 CONICET Digital CONICET |
| url |
http://hdl.handle.net/11336/291534 |
| identifier_str_mv |
Olazábal, Sabrina Ximena; Tunik, Maisa Andrea; Paredes, José Matildo; Allard, Jose Oscar; Foix, Nicolas; The Chubut Group (Cretaceous, Golfo San Jorge Basin): A synthesis of its sedimentary petrography; Asociación Argentina de Sedimentología; Latin American Journal of Sedimentology and Basin Analysis; 32; 1; 7-2025; 44-56 1851-4979 CONICET Digital CONICET |
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eng |
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eng |
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Asociación Argentina de Sedimentología |
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Asociación Argentina de Sedimentología |
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dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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