WebThe shallow subsurface at Ocean Cay on western Great Bahama Bank consists of Pleis- tocene oolitic sand shoals and adjacent facies that exhibit facies-dependent petrophysical heterogeneity and... WebThe origin of these porous trends is related to the depositional and diagenetic history of upper Smackover carbonates and overlying Buckner evaporites. Shoal water oolitic and peloidal grainstones of the upper Smackover were deposited across basement and salt-related topographic highs.
Oolite - Wikipedia
Web2 de ago. de 2012 · The oolitic shoals of the Triassic carbonate platform margin in the Yudongzi (鱼洞子) outcrop of Erlangmiao (二郎庙) area in the northwestern Sichuan (四 … Web24 de abr. de 2024 · 3.3.2. arenite shoals. The lithology of arenite shoals is mainly sparry calcarenite. The pores are mainly mold pores and intragranular pores. The porosity is high. The lateral change is fast. Reservoirs in arenite shoals are classified as Class I reservoirs (Figure 5). Figure 4. Markers of oolitic shoal facies of B5 in Well X-5. Figure 5. church of ubuntu wellness clinic
Distribution patterns and controlling factors for reservoir ...
Web24 de mar. de 2024 · There exist three stages of high-energy slope break belts in the Feixianguan period, the corresponding three stages of oolitic shoals gradually migrating … Web1 de set. de 2016 · Modern tidally dominated marginal oolitic shoals of the Bahamas provided detailed information on spatial patterns and geometries of ooid sand bodies (Harris, 2010, Harris et al., 2011), geometry of bedforms and their relationship to tidal currents (Gonzalez and Eberli, 1997, Reeder and Rankey, 2008, Rankey and Reeder, 2012), … WebThis new sedimentary model can not only determine the formation period and distribution of oolitic shoals with high-quality reservoir, but also provides a new exploration direction for the shallow water ramp on the southeast side of the trough with low exploration. 1887. search. search ADVANCED SEARCH account_circle; dewey leboeuf collapse