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dc.contributor.author
Schwarz, Ernesto
dc.contributor.author
Veiga, Gonzalo Diego
dc.contributor.author
Álvarez Trentini, Gastón
dc.contributor.author
Isla, Manuel Fermín
dc.date.available
2023-08-03T14:41:41Z
dc.date.issued
2018
dc.identifier.citation
Expanding the spectrum of shallow marine carbonate-siliciclastic systems: processes, facies distribution, and depositional controls of a siliciclastic-dominated example; XX International Sedimentological Congress; Québec; Canadá; 2018; 722-722
dc.identifier.isbn
978-2-89146-937-1
dc.identifier.uri
http://hdl.handle.net/11336/206836
dc.description.abstract
Most of the present knowledge of shallow-marine, mixed carbonate-siliciclastic systems relies on examples from the carbonate-dominated-end of the carbonate-siliciclastic spectrum. This contribution provides a detailed reconstruction of a siliciclastic-dominated mixed system (Pilmatué Member of the Agrio Formation, Neuquén Basin, Argentina) that explores the variability of depositional models and resulting stratigraphic units within these systems. The Pilmatué Memberregressive system comprises a storm-dominated, shoreface-to-basinal setting with three subparallel zones: a distal mixed zone, a middle siliciclastic zone, and a proximal mixed zone. In the latter, a significant proportion of ooids and bioclasts were mixed with terrigenous sediment, supplied mostly via along-shore currents. Storm-generated flows were the primary processes exporting finesand and mud to the middle zone, but were ineffective to remove coarser sediment. The distal zone received low volumes of siliciclastic mud, which mixed with planktonic-derived-carbonate material. Successive events of shoreline progradation and retrogradation of the Pilmatué system generated up to 17 parasequences, which are bounded by shell beds associated with transgressivesurfaces. The facies distribution and resulting genetic units of this iliciclastic-dominated mixed system are markedly different to the ones observed in present and ancient carbonate-dominated mixed systems, but they show strong similarities with the products of storm-dominated, pure siliciclastic shoreface-shelf systems. Basin-scale depositional controls, such as arid climaticconditions and shallow epeiric seas might aid in the development of mixed systems across the full spectrum (i.e., from carbonate- to siliciclastic-dominated end-members), but the interplay of processes supplying sand to the system, as well as processes transporting sediment across the marine environment are key controls in shaping the tridimensional facies distribution and thegenetic units of siliciclastic-dominated mixed systems. Thus, the identification of different combinations of basin-scale factors and depositional processes are key for a better prediction of conventional and unconventional reservoirs within mixed, carbonate-siliciclastic successions worldwide.
dc.format
application/pdf
dc.language.iso
eng
dc.publisher
International Association of Sedimentologists
dc.rights
info:eu-repo/semantics/restrictedAccess
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.subject
Mixed carbonate-siliciclastic systems
dc.subject
Sequence stratigraphy
dc.subject
Pilmatué Member
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
Expanding the spectrum of shallow marine carbonate-siliciclastic systems: processes, facies distribution, and depositional controls of a siliciclastic-dominated example
dc.type
info:eu-repo/semantics/publishedVersion
dc.type
info:eu-repo/semantics/conferenceObject
dc.type
info:ar-repo/semantics/documento de conferencia
dc.date.updated
2022-11-14T15:30:29Z
dc.journal.volume
2
dc.journal.pagination
722-722
dc.journal.pais
Canadá
dc.journal.ciudad
Quebec
dc.description.fil
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
dc.description.fil
Fil: Veiga, Gonzalo Diego. 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
dc.description.fil
Fil: Álvarez Trentini, Gastón. 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
dc.description.fil
Fil: Isla, Manuel Fermín. 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
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://www.sedimentologists.org/isc
dc.conicet.rol
Autor
dc.conicet.rol
Autor
dc.conicet.rol
Autor
dc.conicet.rol
Autor
dc.coverage
Nacional
dc.type.subtype
Congreso
dc.description.nombreEvento
XX International Sedimentological Congress
dc.date.evento
2018-08-13
dc.description.ciudadEvento
Québec
dc.description.paisEvento
Canadá
dc.type.publicacion
Book
dc.description.institucionOrganizadora
International Association of Sedimentologists
dc.source.libro
A sedimentary journey through 3 billion years in the new world: Book of abstracts
dc.date.eventoHasta
2018-08-17
dc.type
Congreso
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