Stratigraphy and sedimentology of the terminal fan of Candeleros Formation (Neuquén group), Lower Cretaceous, Neuquén Basin, provinces of Neuquén and Mendoza, Argentina
- Autores
- Sanchez, Maria Lidia; Asurmendi, Estefania
- Año de publicación
- 2015
- Idioma
- español castellano
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The Candeleros Formation is represented by a succession of deposits that represent terminal fans starting to fill a foreland basin (back-arc) during the Albian. The different sub-environments of the terminal fan suggest low gradients during the onset of deposition of the Río Limay Subgroup (Neuquén Group). The terminal fan system is represented by distributary zone (TF-DZ), distributary zone-base zone (TF-DZBZ) and base zone deposits (TF-BZ). Its most notable feature is the presence of bitumen in “pockets” and scattered in the sandstone channel fill and crevasse splays deposit. In this system the feeder zone of the terminal fan system has not been identified, however, the distribution of architectural elements and paleocurrent data allow us to infer that the catchment area of the backbone would have been located to the NNW/NW. Distributary zone deposits are characterized by thick deposits of low sinuosity channel, with a high degree of connectivity and strong vertical aggradation of channel belts. Deposits of distributary zone-base zone are characterized by a higher density of channel deposits/distributary plain, but with belt channel less thick, longer laterally, greater width/thickness ratio and connectivity in the braided deposits. The distal parts of the terminal fan are well represented and vary only in the channelized deposits and mantle/floodplain ratio, which is abruptly reduced towards the flood basin connection. The importance of Candeleros Formation deposits is that they are remnants of accommodation that preserved the original architecture and represent exhumed reservoirs.
Fil: Sanchez, Maria Lidia. Universidad Nacional de Río Cuarto; Argentina
Fil: Asurmendi, Estefania. Universidad Nacional de Río Cuarto. Facultad de Ciencias Exactas, Fisicoquímicas y Naturales. Departamento de Geología; Argentina - Materia
-
CANDELEROS FORMATION
NEUQUEN BASIN
TERMINAL FAN - 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:11336/69686
Ver los metadatos del registro completo
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Stratigraphy and sedimentology of the terminal fan of Candeleros Formation (Neuquén group), Lower Cretaceous, Neuquén Basin, provinces of Neuquén and Mendoza, ArgentinaEstratigrafía y sedimentología del abanico terminal de la Formación Candeleros (Grupo Neuquén), Cretácico Inferior, Cuenca Neuquina, provincias de Neuquén y Mendoza, ArgentinaSanchez, Maria LidiaAsurmendi, EstefaniaCANDELEROS FORMATIONNEUQUEN BASINTERMINAL FANhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Candeleros Formation is represented by a succession of deposits that represent terminal fans starting to fill a foreland basin (back-arc) during the Albian. The different sub-environments of the terminal fan suggest low gradients during the onset of deposition of the Río Limay Subgroup (Neuquén Group). The terminal fan system is represented by distributary zone (TF-DZ), distributary zone-base zone (TF-DZBZ) and base zone deposits (TF-BZ). Its most notable feature is the presence of bitumen in “pockets” and scattered in the sandstone channel fill and crevasse splays deposit. In this system the feeder zone of the terminal fan system has not been identified, however, the distribution of architectural elements and paleocurrent data allow us to infer that the catchment area of the backbone would have been located to the NNW/NW. Distributary zone deposits are characterized by thick deposits of low sinuosity channel, with a high degree of connectivity and strong vertical aggradation of channel belts. Deposits of distributary zone-base zone are characterized by a higher density of channel deposits/distributary plain, but with belt channel less thick, longer laterally, greater width/thickness ratio and connectivity in the braided deposits. The distal parts of the terminal fan are well represented and vary only in the channelized deposits and mantle/floodplain ratio, which is abruptly reduced towards the flood basin connection. The importance of Candeleros Formation deposits is that they are remnants of accommodation that preserved the original architecture and represent exhumed reservoirs.Fil: Sanchez, Maria Lidia. Universidad Nacional de Río Cuarto; ArgentinaFil: Asurmendi, Estefania. Universidad Nacional de Río Cuarto. Facultad de Ciencias Exactas, Fisicoquímicas y Naturales. Departamento de Geología; ArgentinaServicio Nacional de Geología y Minería2015-09info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/69686Sanchez, Maria Lidia; Asurmendi, Estefania; Stratigraphy and sedimentology of the terminal fan of Candeleros Formation (Neuquén group), Lower Cretaceous, Neuquén Basin, provinces of Neuquén and Mendoza, Argentina ; Servicio Nacional de Geología y Minería; Andean Geology; 42; 3; 9-2015; 329-3480718-70920718-7106CONICET DigitalCONICETspainfo:eu-repo/semantics/altIdentifier/url/http://www.andeangeology.cl/index.php/revista1/article/view/2867info:eu-repo/semantics/altIdentifier/doi/10.5027/andgeoV42n3-a03info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:34:00Zoai:ri.conicet.gov.ar:11336/69686instacron: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 10:34:01.154CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Stratigraphy and sedimentology of the terminal fan of Candeleros Formation (Neuquén group), Lower Cretaceous, Neuquén Basin, provinces of Neuquén and Mendoza, Argentina Estratigrafía y sedimentología del abanico terminal de la Formación Candeleros (Grupo Neuquén), Cretácico Inferior, Cuenca Neuquina, provincias de Neuquén y Mendoza, Argentina |
title |
Stratigraphy and sedimentology of the terminal fan of Candeleros Formation (Neuquén group), Lower Cretaceous, Neuquén Basin, provinces of Neuquén and Mendoza, Argentina |
spellingShingle |
Stratigraphy and sedimentology of the terminal fan of Candeleros Formation (Neuquén group), Lower Cretaceous, Neuquén Basin, provinces of Neuquén and Mendoza, Argentina Sanchez, Maria Lidia CANDELEROS FORMATION NEUQUEN BASIN TERMINAL FAN |
title_short |
Stratigraphy and sedimentology of the terminal fan of Candeleros Formation (Neuquén group), Lower Cretaceous, Neuquén Basin, provinces of Neuquén and Mendoza, Argentina |
title_full |
Stratigraphy and sedimentology of the terminal fan of Candeleros Formation (Neuquén group), Lower Cretaceous, Neuquén Basin, provinces of Neuquén and Mendoza, Argentina |
title_fullStr |
Stratigraphy and sedimentology of the terminal fan of Candeleros Formation (Neuquén group), Lower Cretaceous, Neuquén Basin, provinces of Neuquén and Mendoza, Argentina |
title_full_unstemmed |
Stratigraphy and sedimentology of the terminal fan of Candeleros Formation (Neuquén group), Lower Cretaceous, Neuquén Basin, provinces of Neuquén and Mendoza, Argentina |
title_sort |
Stratigraphy and sedimentology of the terminal fan of Candeleros Formation (Neuquén group), Lower Cretaceous, Neuquén Basin, provinces of Neuquén and Mendoza, Argentina |
dc.creator.none.fl_str_mv |
Sanchez, Maria Lidia Asurmendi, Estefania |
author |
Sanchez, Maria Lidia |
author_facet |
Sanchez, Maria Lidia Asurmendi, Estefania |
author_role |
author |
author2 |
Asurmendi, Estefania |
author2_role |
author |
dc.subject.none.fl_str_mv |
CANDELEROS FORMATION NEUQUEN BASIN TERMINAL FAN |
topic |
CANDELEROS FORMATION NEUQUEN BASIN TERMINAL FAN |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
The Candeleros Formation is represented by a succession of deposits that represent terminal fans starting to fill a foreland basin (back-arc) during the Albian. The different sub-environments of the terminal fan suggest low gradients during the onset of deposition of the Río Limay Subgroup (Neuquén Group). The terminal fan system is represented by distributary zone (TF-DZ), distributary zone-base zone (TF-DZBZ) and base zone deposits (TF-BZ). Its most notable feature is the presence of bitumen in “pockets” and scattered in the sandstone channel fill and crevasse splays deposit. In this system the feeder zone of the terminal fan system has not been identified, however, the distribution of architectural elements and paleocurrent data allow us to infer that the catchment area of the backbone would have been located to the NNW/NW. Distributary zone deposits are characterized by thick deposits of low sinuosity channel, with a high degree of connectivity and strong vertical aggradation of channel belts. Deposits of distributary zone-base zone are characterized by a higher density of channel deposits/distributary plain, but with belt channel less thick, longer laterally, greater width/thickness ratio and connectivity in the braided deposits. The distal parts of the terminal fan are well represented and vary only in the channelized deposits and mantle/floodplain ratio, which is abruptly reduced towards the flood basin connection. The importance of Candeleros Formation deposits is that they are remnants of accommodation that preserved the original architecture and represent exhumed reservoirs. Fil: Sanchez, Maria Lidia. Universidad Nacional de Río Cuarto; Argentina Fil: Asurmendi, Estefania. Universidad Nacional de Río Cuarto. Facultad de Ciencias Exactas, Fisicoquímicas y Naturales. Departamento de Geología; Argentina |
description |
The Candeleros Formation is represented by a succession of deposits that represent terminal fans starting to fill a foreland basin (back-arc) during the Albian. The different sub-environments of the terminal fan suggest low gradients during the onset of deposition of the Río Limay Subgroup (Neuquén Group). The terminal fan system is represented by distributary zone (TF-DZ), distributary zone-base zone (TF-DZBZ) and base zone deposits (TF-BZ). Its most notable feature is the presence of bitumen in “pockets” and scattered in the sandstone channel fill and crevasse splays deposit. In this system the feeder zone of the terminal fan system has not been identified, however, the distribution of architectural elements and paleocurrent data allow us to infer that the catchment area of the backbone would have been located to the NNW/NW. Distributary zone deposits are characterized by thick deposits of low sinuosity channel, with a high degree of connectivity and strong vertical aggradation of channel belts. Deposits of distributary zone-base zone are characterized by a higher density of channel deposits/distributary plain, but with belt channel less thick, longer laterally, greater width/thickness ratio and connectivity in the braided deposits. The distal parts of the terminal fan are well represented and vary only in the channelized deposits and mantle/floodplain ratio, which is abruptly reduced towards the flood basin connection. The importance of Candeleros Formation deposits is that they are remnants of accommodation that preserved the original architecture and represent exhumed reservoirs. |
publishDate |
2015 |
dc.date.none.fl_str_mv |
2015-09 |
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/11336/69686 Sanchez, Maria Lidia; Asurmendi, Estefania; Stratigraphy and sedimentology of the terminal fan of Candeleros Formation (Neuquén group), Lower Cretaceous, Neuquén Basin, provinces of Neuquén and Mendoza, Argentina ; Servicio Nacional de Geología y Minería; Andean Geology; 42; 3; 9-2015; 329-348 0718-7092 0718-7106 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/69686 |
identifier_str_mv |
Sanchez, Maria Lidia; Asurmendi, Estefania; Stratigraphy and sedimentology of the terminal fan of Candeleros Formation (Neuquén group), Lower Cretaceous, Neuquén Basin, provinces of Neuquén and Mendoza, Argentina ; Servicio Nacional de Geología y Minería; Andean Geology; 42; 3; 9-2015; 329-348 0718-7092 0718-7106 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
spa |
language |
spa |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/http://www.andeangeology.cl/index.php/revista1/article/view/2867 info:eu-repo/semantics/altIdentifier/doi/10.5027/andgeoV42n3-a03 |
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 |
dc.publisher.none.fl_str_mv |
Servicio Nacional de Geología y Minería |
publisher.none.fl_str_mv |
Servicio Nacional de Geología y Minería |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
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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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13.070432 |