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dc.contributor.author
Ponce, Juan Jose  
dc.contributor.author
Carmona, Noelia Beatriz  
dc.contributor.author
Jait, Damián  
dc.contributor.author
Cevallos, Martín  
dc.contributor.author
Rojas, Christian  
dc.date.available
2024-01-24T15:11:11Z  
dc.date.issued
2023-07  
dc.identifier.citation
Ponce, Juan Jose; Carmona, Noelia Beatriz; Jait, Damián; Cevallos, Martín; Rojas, Christian; Sedimentological and ichnological characterization of delta front mouth bars in a river-dominated delta (Upper Cretaceous) from the La Anita Formation, Austral Basin, Argentina; Wiley Blackwell Publishing, Inc; Sedimentology; 71; 1; 7-2023; 27-53  
dc.identifier.issn
0037-0746  
dc.identifier.uri
http://hdl.handle.net/11336/224706  
dc.description.abstract
Integrated sedimentological and ichnological studies in deltaic systems are key to determine whether a delta is river-dominated, tide-dominated, wave-dominated or hybrid, and thus predict the distribution of their geometries and main reservoirs. The Austral Basin is one of the most important oil and gas basins from Argentina, and the Upper Cretaceous La Anita Formation has shown excellent attributes as a hydrocarbon reservoir. Analysis of eleven cores, supplemented by a large volume of well logging data and two-dimensional and three-dimensional seismic, allowed to recognize a river-dominated deltaic system affected by hyperpycnal discharges and storm events. Four main facies associations were recognized (offshore, prodelta, delta front and interdistributary bay), being the delta front facies associations, the most recurrent facies and constituting the major reservoir of the La Anita Formation. Three types of deltaic mouth bars have been characterized in the delta front. Type I corresponds to active mouth bars with preservation of sedimentary structures and bioturbated by suspension and deposit feeding organisms. Type II represents the stopped progradation and the abandonment in the construction of mouth bars, which are completely reworked by suspension and deposit feeding organisms and, in some cases, affected by fair-weather or storm-wave processes at the top. Type III comprises hyperpycnal mouth bars characterized by transitional and recurrent intervals of sedimentary structures, high concentration of phytodetritus, and paucity of bioturbation. The amalgamation and coalescence of these three types of sandy mouth bars produce lobe-like geometries and are the main processes of delta front construction and progradation. This proposed model allows to explain the principal mechanism of construction of the delta front and can be applied to the analysis of other reservoirs where mouth bar architectural elements are dominant.  
dc.format
application/pdf  
dc.language.iso
eng  
dc.publisher
Wiley Blackwell Publishing, Inc  
dc.rights
info:eu-repo/semantics/restrictedAccess  
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/  
dc.subject
AUSTRAL BASIN  
dc.subject
CRETACEOUS  
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HYPERPYCNITES  
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ICHNOLOGY  
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MOUTH BAR  
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RIVER-DOMINATED DELTA  
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SEDIMENTOLOGY  
dc.subject.classification
Geología  
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Ciencias de la Tierra y relacionadas con el Medio Ambiente  
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CIENCIAS NATURALES Y EXACTAS  
dc.title
Sedimentological and ichnological characterization of delta front mouth bars in a river-dominated delta (Upper Cretaceous) from the La Anita Formation, Austral Basin, Argentina  
dc.type
info:eu-repo/semantics/article  
dc.type
info:ar-repo/semantics/artículo  
dc.type
info:eu-repo/semantics/publishedVersion  
dc.date.updated
2024-01-22T12:51:51Z  
dc.journal.volume
71  
dc.journal.number
1  
dc.journal.pagination
27-53  
dc.journal.pais
Reino Unido  
dc.journal.ciudad
Londres  
dc.description.fil
Fil: Ponce, Juan Jose. Secretaría de Industria y Minería. Servicio Geológico Minero Argentino; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Confluencia; Argentina. Universidad Nacional de Río Negro. Sede Alto Valle; Argentina  
dc.description.fil
Fil: Carmona, Noelia Beatriz. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigación en Paleobiología y Geología; Argentina. Universidad Nacional de Río Negro. Sede Alto Valle; Argentina  
dc.description.fil
Fil: Jait, Damián. No especifíca;  
dc.description.fil
Fil: Cevallos, Martín. No especifíca;  
dc.description.fil
Fil: Rojas, Christian. No especifíca;  
dc.journal.title
Sedimentology  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://onlinelibrary.wiley.com/doi/10.1111/sed.13127  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1111/sed.13127