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
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/69686
Acceder
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spelling 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 Técnicas2025-10-22T12:06:30Zoai: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:34982025-10-22 12:06:30.331CONICET 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
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 12.982451

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