Can polygonal faults help locate deep-water reservoirs? (Record no. 188661)

MARC details
000 -LEADER
fixed length control field 02440nab a2200229 4500
008 - CÓDIGOS DE INFORMACIÓN DE LONGITUD FIJA - INFORMACIÓN GENERAL
Campo de control de longitud fija 260224s2014 xxu ing
041 ## - IDIOMA
Idioma Inglés
245 00 - TITULO
Título Can polygonal faults help locate deep-water reservoirs?
260 ## - PUBLICACION, DISTRIBUCION, ETC
Lugar de publicación, distribución, etc.
Nombre de publicador, distribuidor, etc.
Fecha de publicación, distribución, etc. sept. 2014
270 ## - FECHA DE CARGA
Fecha de carga 20/11/2014 ; 20/11/2014
300 ## - DESCRIPCION FISICA
Otra extensión 21 p. ; 1717-1738
520 ## - RESUMEN, ETC
Resumen Transcripción del resumen del autor: Polygonal faults are compaction-related normal faults that develop in very fine-grained sedimentary successions. Despite their ubiquity, few studies have highlighted the application of polygonal fault mapping to identifying deep-water sandstone reservoirs. We use three-dimensional seismic and borehole data from the Måløy slope, offshore Norway to demonstrate that the distribution, cross-sectional geometry, and throw characteristics of polygonal faults can be used to locate deep-water sandstone reservoirs. We identify two tiers of polygonal faults in the Cretaceous to lower Paleogene succession. The lowermost tier is stratigraphically restricted to the lower Barremian-to-lowermost Turonian succession and likely formed during the early Turonian. The uppermost tier spans the entire Cretaceous succession and likely formed during the Maastrichtian. An abrupt decrease in the thickness of the upper tier occurs where a 92-m (302-ft) thick, sandstone-rich slope fan is developed in the upper Turonian interval. Furthermore, the lower tips of faults in the upper tier, which are defined by anomalously high throw gradients, cluster at the top of the sandstone, resulting in decoupling of this tier from the underlying, lower Turonian tier. We interpret that faults in the upper tier nucleated above the reservoir across the entire slope and that the slope-fan sandstone acted as a mechanical barrier to downward fault propagation, resulting in abrupt thinning of the tier at the sandstone pinchout. We demonstrate polygonal faults are not simply an academic curiosity; mapping of these enigmatic structures can have practical applications for the delineation of a variety of reservoir types in hydrocarbon-bearing sedimentary basins worldwide.
581 ## - ESTADO DE COLECCIÓN
Estado de colección 9
773 0# - CORRECCIÓN
Título AAPG Bulletin
Partes relacionadas 98
942 ## - DESC. DE MATERIAL
Tipo de item KOHA Artículo de Revista
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Jackson, Christopher A.L.
9 (RLIN) 49704
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Carruthers, Daniel T.
9 (RLIN) 54235
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Mahlo, Seshane N.
9 (RLIN) 54236
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Briggs, Omieari
9 (RLIN) 54237
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 200060867   200060867 06/03/2026 Artículo de Revista


Instituto Argentino del Petróleo y del Gas
Maipú 639 (C1006ACG) – Buenos Aires – Argentina
Tel: (54 11) 5277 IAPG (4274)
Lu - Vie 11 a 17 hs
Mail: biblio@iapg.org.ar


Copyright © 2026, Instituto Argentino del Petróleo y del Gas, todos los derechos reservados.

Protección de datos personales