Evolving fill‐and‐spill patterns across linked early post‐rift depocentres control lobe characteristics: Los Molles Formation, Argentina
- Autores
- Privat, Aurélia M. L.; Peakall, Jeff; Hodgson, David M.; Schwarz, Ernesto; Jackson, Christopher A. L.; Arnol, Jonatan Ariel
- Año de publicación
- 2024
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Inherited rift topography controls the sediment routeing, timing of sand supply, and sedimentary linkage of early post-rift depocentres. Exhumed examples of early post-rift turbidite systems are rare and previous studies have examined the evolution of individual depocentres; in contrast, the detailed evolution of early post-rift turbidite systems across multiple depocentres has never been documented. Current fill-and-spill models do not detail the stratigraphic architecture and evolution of sedimentological characteristics of multiple intraslope fans developed across topography, including bed type distributions. Here, the evolution of three intraslope fans that developed across two early post-rift depocentres is documented along an 18 km-long transect in the southern Neuquén Basin, Argentina. The relative chronology of sand supply in depocentres is constrained with new U-Pb ages, and sediment source areas with provenance analysis. The early post-rift intraslope fans record progradation of the system and progressive sedimentary linkage of post-rift depocentres, transverse to local syn-rift structures, with sediment routeing subparallel to the cratonic basin margin. The large-scale stratigraphic architecture of intraslope fans indicates an evolution as a fill-and-spill system, with initial confinement through flow stripping and overspill to spillover with erosion and bypass across a transverse topographic high separating the depocentres. Changes in early post-rift intraslope fan characteristics, including thickness, sandstone content, lobe complex stacking patterns, stratal termination patterns, and bed type distribution, record changing confinement through time within a depocentre, and spatially across depocentres. The strong spatial and vertical stratigraphic variability of transitional flow deposits and hybrid event beds reflects enhanced erosion, sediment bypass and flow transformation across transverse relief between the two depocentres during the spillover phase. These findings advance our understanding of early post-rift turbidite systems and refine fill-and-spill models, which will help the prediction of spatial and vertical changes in rock quality and connectivity in subsurface hydrocarbon reservoirs and CO2 storage sites.
Fil: Privat, Aurélia M. L.. University of Leeds; Reino Unido
Fil: Peakall, Jeff. University of Leeds; Reino Unido
Fil: Hodgson, David M.. University of Leeds; Reino Unido
Fil: Schwarz, Ernesto. 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: Jackson, Christopher A. L.. Imperial College London; Reino Unido
Fil: Arnol, Jonatan Ariel. 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 - Materia
-
EARLY POST-RIFT
INTRASLOPE LOBES
FILL-AND-SPILL
NEUQUEN BASIN - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/238743
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spelling |
Evolving fill‐and‐spill patterns across linked early post‐rift depocentres control lobe characteristics: Los Molles Formation, ArgentinaPrivat, Aurélia M. L.Peakall, JeffHodgson, David M.Schwarz, ErnestoJackson, Christopher A. L.Arnol, Jonatan ArielEARLY POST-RIFTINTRASLOPE LOBESFILL-AND-SPILLNEUQUEN BASINhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Inherited rift topography controls the sediment routeing, timing of sand supply, and sedimentary linkage of early post-rift depocentres. Exhumed examples of early post-rift turbidite systems are rare and previous studies have examined the evolution of individual depocentres; in contrast, the detailed evolution of early post-rift turbidite systems across multiple depocentres has never been documented. Current fill-and-spill models do not detail the stratigraphic architecture and evolution of sedimentological characteristics of multiple intraslope fans developed across topography, including bed type distributions. Here, the evolution of three intraslope fans that developed across two early post-rift depocentres is documented along an 18 km-long transect in the southern Neuquén Basin, Argentina. The relative chronology of sand supply in depocentres is constrained with new U-Pb ages, and sediment source areas with provenance analysis. The early post-rift intraslope fans record progradation of the system and progressive sedimentary linkage of post-rift depocentres, transverse to local syn-rift structures, with sediment routeing subparallel to the cratonic basin margin. The large-scale stratigraphic architecture of intraslope fans indicates an evolution as a fill-and-spill system, with initial confinement through flow stripping and overspill to spillover with erosion and bypass across a transverse topographic high separating the depocentres. Changes in early post-rift intraslope fan characteristics, including thickness, sandstone content, lobe complex stacking patterns, stratal termination patterns, and bed type distribution, record changing confinement through time within a depocentre, and spatially across depocentres. The strong spatial and vertical stratigraphic variability of transitional flow deposits and hybrid event beds reflects enhanced erosion, sediment bypass and flow transformation across transverse relief between the two depocentres during the spillover phase. These findings advance our understanding of early post-rift turbidite systems and refine fill-and-spill models, which will help the prediction of spatial and vertical changes in rock quality and connectivity in subsurface hydrocarbon reservoirs and CO2 storage sites.Fil: Privat, Aurélia M. L.. University of Leeds; Reino UnidoFil: Peakall, Jeff. University of Leeds; Reino UnidoFil: Hodgson, David M.. University of Leeds; Reino UnidoFil: Schwarz, Ernesto. 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: Jackson, Christopher A. L.. Imperial College London; Reino UnidoFil: Arnol, Jonatan Ariel. 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; ArgentinaWiley Blackwell Publishing, Inc2024-06info: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/11336/238743Privat, Aurélia M. L.; Peakall, Jeff; Hodgson, David M.; Schwarz, Ernesto; Jackson, Christopher A. L.; et al.; Evolving fill‐and‐spill patterns across linked early post‐rift depocentres control lobe characteristics: Los Molles Formation, Argentina; Wiley Blackwell Publishing, Inc; Sedimentology; 6-2024; 1-500037-0746CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://onlinelibrary.wiley.com/doi/10.1111/sed.13190info:eu-repo/semantics/altIdentifier/doi/10.1111/sed.13190info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:08:58Zoai:ri.conicet.gov.ar:11336/238743instacron: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 10:08:58.543CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Evolving fill‐and‐spill patterns across linked early post‐rift depocentres control lobe characteristics: Los Molles Formation, Argentina |
title |
Evolving fill‐and‐spill patterns across linked early post‐rift depocentres control lobe characteristics: Los Molles Formation, Argentina |
spellingShingle |
Evolving fill‐and‐spill patterns across linked early post‐rift depocentres control lobe characteristics: Los Molles Formation, Argentina Privat, Aurélia M. L. EARLY POST-RIFT INTRASLOPE LOBES FILL-AND-SPILL NEUQUEN BASIN |
title_short |
Evolving fill‐and‐spill patterns across linked early post‐rift depocentres control lobe characteristics: Los Molles Formation, Argentina |
title_full |
Evolving fill‐and‐spill patterns across linked early post‐rift depocentres control lobe characteristics: Los Molles Formation, Argentina |
title_fullStr |
Evolving fill‐and‐spill patterns across linked early post‐rift depocentres control lobe characteristics: Los Molles Formation, Argentina |
title_full_unstemmed |
Evolving fill‐and‐spill patterns across linked early post‐rift depocentres control lobe characteristics: Los Molles Formation, Argentina |
title_sort |
Evolving fill‐and‐spill patterns across linked early post‐rift depocentres control lobe characteristics: Los Molles Formation, Argentina |
dc.creator.none.fl_str_mv |
Privat, Aurélia M. L. Peakall, Jeff Hodgson, David M. Schwarz, Ernesto Jackson, Christopher A. L. Arnol, Jonatan Ariel |
author |
Privat, Aurélia M. L. |
author_facet |
Privat, Aurélia M. L. Peakall, Jeff Hodgson, David M. Schwarz, Ernesto Jackson, Christopher A. L. Arnol, Jonatan Ariel |
author_role |
author |
author2 |
Peakall, Jeff Hodgson, David M. Schwarz, Ernesto Jackson, Christopher A. L. Arnol, Jonatan Ariel |
author2_role |
author author author author author |
dc.subject.none.fl_str_mv |
EARLY POST-RIFT INTRASLOPE LOBES FILL-AND-SPILL NEUQUEN BASIN |
topic |
EARLY POST-RIFT INTRASLOPE LOBES FILL-AND-SPILL NEUQUEN 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 |
Inherited rift topography controls the sediment routeing, timing of sand supply, and sedimentary linkage of early post-rift depocentres. Exhumed examples of early post-rift turbidite systems are rare and previous studies have examined the evolution of individual depocentres; in contrast, the detailed evolution of early post-rift turbidite systems across multiple depocentres has never been documented. Current fill-and-spill models do not detail the stratigraphic architecture and evolution of sedimentological characteristics of multiple intraslope fans developed across topography, including bed type distributions. Here, the evolution of three intraslope fans that developed across two early post-rift depocentres is documented along an 18 km-long transect in the southern Neuquén Basin, Argentina. The relative chronology of sand supply in depocentres is constrained with new U-Pb ages, and sediment source areas with provenance analysis. The early post-rift intraslope fans record progradation of the system and progressive sedimentary linkage of post-rift depocentres, transverse to local syn-rift structures, with sediment routeing subparallel to the cratonic basin margin. The large-scale stratigraphic architecture of intraslope fans indicates an evolution as a fill-and-spill system, with initial confinement through flow stripping and overspill to spillover with erosion and bypass across a transverse topographic high separating the depocentres. Changes in early post-rift intraslope fan characteristics, including thickness, sandstone content, lobe complex stacking patterns, stratal termination patterns, and bed type distribution, record changing confinement through time within a depocentre, and spatially across depocentres. The strong spatial and vertical stratigraphic variability of transitional flow deposits and hybrid event beds reflects enhanced erosion, sediment bypass and flow transformation across transverse relief between the two depocentres during the spillover phase. These findings advance our understanding of early post-rift turbidite systems and refine fill-and-spill models, which will help the prediction of spatial and vertical changes in rock quality and connectivity in subsurface hydrocarbon reservoirs and CO2 storage sites. Fil: Privat, Aurélia M. L.. University of Leeds; Reino Unido Fil: Peakall, Jeff. University of Leeds; Reino Unido Fil: Hodgson, David M.. University of Leeds; Reino Unido Fil: Schwarz, Ernesto. 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: Jackson, Christopher A. L.. Imperial College London; Reino Unido Fil: Arnol, Jonatan Ariel. 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 |
description |
Inherited rift topography controls the sediment routeing, timing of sand supply, and sedimentary linkage of early post-rift depocentres. Exhumed examples of early post-rift turbidite systems are rare and previous studies have examined the evolution of individual depocentres; in contrast, the detailed evolution of early post-rift turbidite systems across multiple depocentres has never been documented. Current fill-and-spill models do not detail the stratigraphic architecture and evolution of sedimentological characteristics of multiple intraslope fans developed across topography, including bed type distributions. Here, the evolution of three intraslope fans that developed across two early post-rift depocentres is documented along an 18 km-long transect in the southern Neuquén Basin, Argentina. The relative chronology of sand supply in depocentres is constrained with new U-Pb ages, and sediment source areas with provenance analysis. The early post-rift intraslope fans record progradation of the system and progressive sedimentary linkage of post-rift depocentres, transverse to local syn-rift structures, with sediment routeing subparallel to the cratonic basin margin. The large-scale stratigraphic architecture of intraslope fans indicates an evolution as a fill-and-spill system, with initial confinement through flow stripping and overspill to spillover with erosion and bypass across a transverse topographic high separating the depocentres. Changes in early post-rift intraslope fan characteristics, including thickness, sandstone content, lobe complex stacking patterns, stratal termination patterns, and bed type distribution, record changing confinement through time within a depocentre, and spatially across depocentres. The strong spatial and vertical stratigraphic variability of transitional flow deposits and hybrid event beds reflects enhanced erosion, sediment bypass and flow transformation across transverse relief between the two depocentres during the spillover phase. These findings advance our understanding of early post-rift turbidite systems and refine fill-and-spill models, which will help the prediction of spatial and vertical changes in rock quality and connectivity in subsurface hydrocarbon reservoirs and CO2 storage sites. |
publishDate |
2024 |
dc.date.none.fl_str_mv |
2024-06 |
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/11336/238743 Privat, Aurélia M. L.; Peakall, Jeff; Hodgson, David M.; Schwarz, Ernesto; Jackson, Christopher A. L.; et al.; Evolving fill‐and‐spill patterns across linked early post‐rift depocentres control lobe characteristics: Los Molles Formation, Argentina; Wiley Blackwell Publishing, Inc; Sedimentology; 6-2024; 1-50 0037-0746 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/238743 |
identifier_str_mv |
Privat, Aurélia M. L.; Peakall, Jeff; Hodgson, David M.; Schwarz, Ernesto; Jackson, Christopher A. L.; et al.; Evolving fill‐and‐spill patterns across linked early post‐rift depocentres control lobe characteristics: Los Molles Formation, Argentina; Wiley Blackwell Publishing, Inc; Sedimentology; 6-2024; 1-50 0037-0746 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://onlinelibrary.wiley.com/doi/10.1111/sed.13190 info:eu-repo/semantics/altIdentifier/doi/10.1111/sed.13190 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
Wiley Blackwell Publishing, Inc |
publisher.none.fl_str_mv |
Wiley Blackwell Publishing, Inc |
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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1844613963035181056 |
score |
13.070432 |