--> Characterization of Pore-Throat Structure and Prediction of Sweet Spots of the Eocene Low Permeability-Tight Beach-Bar Sandstone Reservoirs in the Dongying Depression, Bohai Bay Basin, China
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Characterization of Pore-Throat Structure and Previous HitPredictionNext Hit of Sweet Spots of the Eocene Low Previous HitPermeabilityNext Hit-Tight Beach-Bar Previous HitSandstoneNext Hit Reservoirs in the Dongying Depression, Bohai Bay Basin, China

Abstract

Pore-throat structure is one of the dominant factors controlling the reservoir quality and development benefit of low Previous HitpermeabilityNext Hit-tight Previous HitsandstoneNext Hit reservoirs. The characteristics, distribution and its control on reservoir quality of pore-throat structure of the Eocene low Previous HitpermeabilityNext Hit-tight Previous HitsandstoneNext Hit reservoirs were carefully studied based on the systematically analyses of thin sections, Previous HitporosityNext Hit and Previous HitpermeabilityNext Hit, high pressure mercury, and constant velocity mercury. The low Previous HitpermeabilityNext Hit-tight reservoirs consist of micron-nano scale pore-throats. With the decreasing Previous HitpermeabilityNext Hit the content of nano scale pore-throats increases gradually and the sensitive pore-throat radius of Previous HitpermeabilityNext Hit decrease gradually. A small amount of large scale pore-throats control the Previous HitpermeabilityNext Hit, while the majority small scale pore-throats contribute the Previous HitpermeabilityNext Hit less but control the Previous HitporosityNext Hit more. Normal low-Previous HitpermeabilityNext Hit reservoirs (10-50mD) consist of micron scale pore-throats, which is contributed by pore-throats with radius more than 3μm. Ultra low-Previous HitpermeabilityTop reservoirs (1-10mD) consist of micron-nano scale pore-throats, which is contributed by pore-throats with radius between 1-3μm. Tight reservoirs (<1mD) consist of nano scale pore-throats, which is contributed by pore-throats with radius less than 1μm. The reservoir quality index (RQI) was employed to characterize the pore-throat structures based on the analysis of applicability of macro petrophysical parameters. The larger the number of RQI, the better the pore-throat structure. Affected by the compaction and cooperative diagenesis of sandstone-mudstone interlayers the RQI generally increases gradually with the increase of distance to the sandstone-mudstone contacts in sandstones in the same depth ranges. For a fixed distance to the sandstone-mudstone contact the RQI decreases gradually with the increasing depth. According to these varied characteristics the plate of RQI verified with depth and distance to the sandstone-mudstone contact was determined. The RQI=0.25 is the lower cutoff of the petrophysical-oiliness sweet sport based on the correlation of RQI and reservoir oiliness. Reservoir spaces of sweet sport are dominated by intergranuler pores. The maximum connective pore-throat radius range from 1.47 to 10.5μm with average of 4.92μm. The average pore-throat radius are between 0.17-4.41μm with average of 1.1μm. With the increase of burial depth the thickness of developing sweet sport increase gradually.