Sedimentological and ichnological characterization of delta front mouth bars in a river‐dominated delta (Upper Cretaceous) from the La Anita Formation, Austral Basin, Argentina

Author:

Ponce Juan José123ORCID,Carmona Noelia345ORCID,Jait Damián6,Cevallos Martín6,Rojas Christian6

Affiliation:

1. Consejo Nacional de Investigaciones Científicas y Técnicas, Centro Cientifico Tecnologico CONICET ‐ Patagonia Confluencia Dr. Ramón 372, piso (PB), Depto A Neuqén R8300 Argentina

2. Servicio Geológico Minero Argentino (SEGEMAR), Centro General Roca, Río Negro, SEGEMAR Regional Sur Independencia 1487, Parque Industrial 1, Casilla Correo 228 General Roca CP 8332 Argentina

3. Universidad Nacional de Río Negro Sede Alto Valle‐Valle Medio, Estados Unidos 750 General Roca Río Negro R8332 Argentina

4. Instituto de Investigación en Paleobiología y Geología, Universidad Nacional de Río Negro Río Negro. Av. Gral. Julio Argentino Roca 1242 General Roca Río Negro R8332 Argentina

5. Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET) Instituto de Investigación en Paleobiología y Geología Río Negro. Av. Gral. Julio Argentino Roca 1242 General Roca Río Negro R8332 Argentina

6. Compañía General de Combustibles S.A. Gerencia de Exploración Honduras 5663, CABA Buenos Aires RC1414BNE Argentina

Abstract

AbstractIntegrated 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.

Funder

Consejo Nacional de Investigaciones Científicas y Técnicas

Publisher

Wiley

Subject

Stratigraphy,Geology,General Medicine

Reference90 articles.

1. Estratigrafía y facies de depósitos marinos profundos del Cretácito Superior, Lago Argentino, Provincia de Santa Cruz;Arbe H.A.;Actas, IX Congreso Geológico Argentino,1984

2. Shrimps and leaves: Phytodetrital pulses and bioturbation in deposits of a river‐dominated delta (Middle Jurassic Lajas Formation, Neuquén Basin, Argentina);Arregui M.G.;Palaeogeograp., Palaeoclimato., Palaeoecol.,2019

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