galley
发表于 2025-3-23 13:40:09
Deltaic Depositional Controls on Clinton Sandstone Reservoirs, Senecaville Gas Field, Guernsey Countvely thin, often below seismic resolution, due to low subsidence rates in these basins. This can decrease the size and continuity of sandstone reservoirs, resulting in small and complex stratigraphic traps. Second, the stratigraphic detail necessary to delineate sandstone bodies requires a significa
ferment
发表于 2025-3-23 15:02:32
Deltaic Reservoirs of the Caño Limón Field, Colombia, South Americanated deltas. In general, the highest quality sands are the distributary channel sands, but these can be very problematic as reservoirs because of their highly limited lateral extent and the marked variation in the type of channel-fill possible. Some channels are filled with coarse-grained high perm
低能儿
发表于 2025-3-23 20:23:37
Fluvial-Estuarine Valley Fill at the Mississippian-Pennsylvanian Unconformity, Main Consolidated Fie(Fig. 13–1). Production has come largely from structural traps at depths of less than 5,500 feet (1,675 m) that collectively contain more than sixty different pay zones ranging in age from Ordovician to Pennsylvanian (Fig. 13–2). Despite the maturity of the basin, significant discoveries could come
AVANT
发表于 2025-3-23 23:50:55
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Cumbersome
发表于 2025-3-24 02:44:04
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Handedness
发表于 2025-3-24 06:45:30
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PSA-velocity
发表于 2025-3-24 11:54:02
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外形
发表于 2025-3-24 15:43:08
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条约
发表于 2025-3-24 19:50:50
Book 19901st editione studies involving a variety of depositional settings, tectonic provinces, and burial/diagenetic histories emphasize depositional controls on reservoir architecture, petrophysical properties, and production performance. An introductory section provides perspective to the nature of reservoir charact
Glower
发表于 2025-3-25 02:34:26
A Braided Fluvial Reservoir, Peco Field, Alberta, Canadaional factors, principally grain size. The finer-grained sandstones have been compacted and cemented to the point of almost totally eliminating porosity, whereas the conglomeratic sandstones retained their depositional porosity and permeability and now are the main reservoir facies.