Estudio cronoestratigráfico y evolución paleoambiental del jurásico inferior-medio en el engolfamiento de la Cuenca Neuquina (Record no. 193159)

MARC details
000 -LEADER
fixed length control field 03025nab a2200289 4500
008 - CÓDIGOS DE INFORMACIÓN DE LONGITUD FIJA - INFORMACIÓN GENERAL
Campo de control de longitud fija 260224s2019 xxu esp
041 ## - IDIOMA
Idioma Español
245 00 - TITULO
Título Estudio cronoestratigráfico y evolución paleoambiental del jurásico inferior-medio en el engolfamiento de la Cuenca Neuquina
260 ## - PUBLICACION, DISTRIBUCION, ETC
Lugar de publicación, distribución, etc.
Nombre de publicador, distribuidor, etc.
Fecha de publicación, distribución, etc. 2019
270 ## - FECHA DE CARGA
Fecha de carga 24/06/2022 ; 15/10/2019
300 ## - DESCRIPCION FISICA
Otra extensión 14 p. ; 110-124
520 ## - RESUMEN, ETC
Resumen The early-middle Jurassic Cuyo Group of the Neuquén Basin is a sedimentary succession of up to 2500 m thick, it shows significant variations from deep-marine, shelf margin to inner-shelf deltaic and fluvial systems. An integrated understanding of the sedimentary system/faciesdistribution in a regional framework is essential to identify potential gas targets. This study discusses the impact of aregional conceptual model on the potential development of this unit at exploration and development scales.A basin scale interpretation was performed on the integration of an extensive subsurface database including 15000 km2 of 3D seismic surveys and available well data such as cores, logs, thin sections, biostratigraphy, zircon/datingand production data. Ten depositional prograding seismic cycles were identified. Each cycle exhibits a different shelf-to-slope arrangement as the basin progressively got filled in a northwest/west direction. Paleogeography andfacies distribution evolved through time from a shallow, low- gradient ramp setting during early basin configuration, to a well-defined shelf-to-slope profile that persisted until the basin shrink age.Four regional schematic cross-sections show the main stratigraphic discontinuities, variations of internal geometrieswithin each cycle, and changes in the supply-accommodation space relationships. These sections together with theisochronous maps of each cycle were used as inputs to build regional facies maps that document the evolution of thesedimentary infill. Outcrops located in the western margin of the Neuquén Basin show a complete source-to-sink profile, providing an analog to validate the interpretation of the subsurface conceptual model. Biostratigraphyand zircon dating linked outcrop and subsurface time intervals.The proposed conceptual model shows the chronostratigraphic relationships between deep-marine,shelf-margin and continental facies of the Cuyo Group at the basin scale. This model will open new exploration and development opportunities for this gas system.
581 ## - ESTADO DE COLECCIÓN
Estado de colección 1
773 0# - CORRECCIÓN
Título Petrotecnia
Partes relacionadas
942 ## - DESC. DE MATERIAL
Tipo de item KOHA Artículo de Revista
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Brinkworth, Walter
9 (RLIN) 683
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Vocaturo, Griselda
9 (RLIN) 55704
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Loss, María Laura
9 (RLIN) 51902
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Mortaloni, Enrique Matías
9 (RLIN) 58792
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Giunta, David Lorenzo
9 (RLIN) 58793
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Massaferro, Enrique Matías
9 (RLIN) 59205
650 #0 - MATERIA
Término tópico Mapas de facies
9 (RLIN) 3146
650 #0 - MATERIA
Término tópico Cronoestratigrafía
9 (RLIN) 26339
856 ## - LINK
Link <a href="https://biblioteca.iapg.org.ar/ArchivosAdjuntos/Conexplor2018/1664.pdf">https://biblioteca.iapg.org.ar/ArchivosAdjuntos/Conexplor2018/1664.pdf</a>
Holdings
Biblioteca propietaria Biblioteca actual Fecha de adquisición Inventario Total de préstamos Inventario Fecha de carga Tipo de item KOHA
Colección Digital IAPG Colección Digital IAPG 06/03/2026 200065473   200065473 06/03/2026 Artículo de Revista


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