Quantification of static connectivity between deep-water channels and stratigraphicically adjacent architectural elements using outcrop analogs (Record no. 187141)

MARC details
000 -LEADER
fixed length control field 02487nab a2200205 4500
008 - CÓDIGOS DE INFORMACIÓN DE LONGITUD FIJA - INFORMACIÓN GENERAL
Campo de control de longitud fija 260224s2012 xxu
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Funk, Jonathan E.
9 (RLIN) 52551
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Slatt, Roger M.
9 (RLIN) 13386
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Pyles, David R.
9 (RLIN) 39764
245 00 - TITULO
Título Quantification of static connectivity between deep-water channels and stratigraphicically adjacent architectural elements using outcrop analogs
260 ## - PUBLICACION, DISTRIBUCION, ETC
Fecha de publicación, distribución, etc. feb. 2012
270 ## - FECHA DE CARGA
Fecha de carga 07/05/2012 ; 07/05/2012
300 ## - DESCRIPCION FISICA
Otra extensión 23 p. ; 277-300
520 ## - RESUMEN, ETC
Resumen Transcripción del resumen del autor: This article uses data from well-exposed outcrops and published information to document static connectivity in deep-water channelized systems. Two measures of static reservoir connectivity on outcrop analogs are proposed: margin connectivity and sand-on-sand connectivity. Margin connectivity (Cm) is the length between two stratigraphically adjacent elements not obstructed by a barrier normalized by the total length of the interface. Sand-on-sand connectivity (Cs) is the length of sand-on-sand contacts between two stratigraphically adjacent elements normalized by the total length of the interface. The Cm and Cs are analyzed with regard to four categories: (1) association of architectural elements, (2) stacking pattern of channel elements, (3) setting on the slope-to-basin profile, and (4) net sand content. Results are as follows. First, connectivity varies by association of architectural elements. Channel-lobe contacts have higher Cm and Cs than channel-channel and channel-levee contacts. Second, connectivity varies by stacking pattern of channel elements. Predominantly vertically stacked channel elements have higher Cm and Cs than predominantly laterally stacked channel elements. Also, disorganized nonsequentially stacked channel elements have higher Cm than organized systematically stacked channel elements. Third, connectivity varies by setting on the slope-to-basin profile. Channel elements in confined settings have higher Cm than both weakly confined and unconfined-distributive settings. Fourth, connectivity varies by net sand content. Channel elements with a high net sand content have higher Cm than those with a low net sand content. Therefore, knowledge of a reservoir's placement in these categories can be used to aid in the prediction of static connectivity.
581 ## - ESTADO DE COLECCIÓN
Estado de colección 2
773 0# - CORRECCIÓN
Título AAPG Bulletin
Partes relacionadas 96
942 ## - DESC. DE MATERIAL
Tipo de item KOHA Artículo de Revista
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 200059247   200059247 06/03/2026 Artículo de Revista


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