Three-dimensional paleomorphologic reconstruction and turbidite distribution prediction revealing a Pleistocene confined basin system in the northeast Nankai Trough area (Record no. 187784)

MARC details
000 -LEADER
fixed length control field 02359nab a2200241 4500
008 - CÓDIGOS DE INFORMACIÓN DE LONGITUD FIJA - INFORMACIÓN GENERAL
Campo de control de longitud fija 260224s2013 xxu ing
041 ## - IDIOMA
Idioma Inglés
245 00 - TITULO
Título Three-dimensional paleomorphologic reconstruction and turbidite distribution prediction revealing a Pleistocene confined basin system in the northeast Nankai Trough area
260 ## - PUBLICACION, DISTRIBUCION, ETC
Lugar de publicación, distribución, etc.
Nombre de publicador, distribuidor, etc.
Fecha de publicación, distribución, etc. mayo 2013
270 ## - FECHA DE CARGA
Fecha de carga 25/06/2013 ; 25/06/2013
300 ## - DESCRIPCION FISICA
Otra extensión 17 p. ; 781-798
520 ## - RESUMEN, ETC
Resumen Transcripción del resumen del autor: Integrated three-dimensional (3-D) paleomorphologic and sedimentary modeling was used to predict the basin architecture and depositional pattern of Pleistocene forearc basin turbidites in a gas hydrate field along the northeast Nankai Trough, off central Japan. Structural unfolding and stratigraphic decompaction of the targeted stratigraphic unit resulted in successful modeling of the paleobathymetry at the time of deposition. This paleobathymetry was characterized by a simple U-shaped paleominibasin. Subsequent turbidity current modeling on the reconstructed paleobathymetric surface demonstrated morphologically controlled turbidity current behavior and selective turbidite sand distribution within the minibasin, which strongly suggests the development of a confined turbidite system. Among three candidate inflow patterns, a northeasterly inflow pattern was determined as most likely. In this scenario, flow reflection and deflection caused ponding and a concentration of sandy turbidite accumulation in the basin center, which facilitated filling of the minibasin. Such a sedimentary character is undetected by seismic data in the studied gas hydrate reservoir formation because of hydrate-cementation–induced seismic anomalies. Our model suggests that 3-D horizon surfaces mapped from 3-D seismic data along with well-log data can be used to predict paleobasin characteristics and depositional processes in deep-water turbidite systems even if seismic profiles cannot be determined because of the presence of gas hydrates.
581 ## - ESTADO DE COLECCIÓN
Estado de colección 5
773 0# - CORRECCIÓN
Título AAPG Bulletin
Partes relacionadas 97
942 ## - DESC. DE MATERIAL
Tipo de item KOHA Artículo de Revista
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Egawa, Kosuke
9 (RLIN) 53341
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Furukawa, Toshiko
9 (RLIN) 53342
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Saeki, Tatsuo
9 (RLIN) 53343
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Suzuki, Kiyofumi
9 (RLIN) 42291
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Narita, Hideo
9 (RLIN) 53344
Holdings
Biblioteca propietaria Biblioteca actual Fecha de adquisición Inventario Total de préstamos Inventario Fecha de carga Tipo de item KOHA
Biblioteca Alejandro Angel Bulgheroni Biblioteca Alejandro Angel Bulgheroni 06/03/2026 200059927   200059927 06/03/2026 Artículo de Revista


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