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Quantitative analysis of geological attributes for reservoir heterogeneity assessment in carbonate sequences; a case from Permian-Triassic reservoirs of the Persian Gulf

机译:碳酸盐序列储层异质性评估地质属性的定量分析; 来自波斯湾的二叠纪三叠系水库的案例

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This study integrates quantitative analysis of reservoir properties with geological parameters to discriminate the reservoir heterogeneities in the Permian-Triassic sequences of the Persian Gulf. To achieve this goal, geological analysis of core samples and thin sections were integrated with petrophysical logs and porosity-permeability data. For quantitative assessment of reservoir heterogeneity, Coefficient of Variation (C-V), Dykstra-Parsons Coefficient (V-DP) and Lorenz Coefficient (V-LC) were used along with the concept of Hydraulic Flow Units (HFU). Depositional facies, diagenetic alterations and sequence stratigraphic framework of the reservoir were used as a basis for the interpretation of geological heterogeneities. Accordingly, 14 microfacies types and 5 facies belts have been defined and indicate a low-angle (homoclinal) ramp model. Complex diagenesis history of these sequences includes marine, hypersaline and shallow to deep burial diagenesis that considerably altered the primary distribution of reservoir properties. A comparison of tested methods revealed that the CV is the best approach for quantification of heterogeneity in targeted reservoir. Consequently, the K4 and K2 are proposed as the most homogeneous units with a dominance of grain-supported facies of shoal setting, intense effects of hypersaline dissolution and lesser effect of compaction and cementation. The K3 and K1 units show high levels of heterogeneity resulting from the combined facies changes and diagenetic alterations (dolomitization, cementation and compaction). Finally, sequence stratigraphic framework of reservoir heterogeneities is discussed for all reservoir units and can be used as a basis for ongoing reservoir studies of the Permian-Triassic sequences in the Persian Gulf and the Middle East.
机译:本研究将储层性质的定量分析与地质参数相结合,以区分波斯湾二叠系-三叠系层序中的储层非均质性。为了实现这一目标,岩芯样品和薄片的地质分析与岩石物理测井和孔隙度-渗透率数据相结合。对于储层非均质性的定量评估,变异系数(C-V)、Dykstra-Parsons系数(V-DP)和Lorenz系数(V-LC)与水力流量单元(HFU)的概念一起使用。储层的沉积相、成岩蚀变和层序地层格架被用作解释地质非均质性的基础。据此,确定了14种微相类型和5个相带,并指示了低角度(同斜)斜坡模型。这些层序的复杂成岩作用历史包括海相成岩作用、高盐成岩作用和浅埋至深埋成岩作用,这些成岩作用极大地改变了储层性质的主要分布。对测试方法的比较表明,CV是量化目标储层非均质性的最佳方法。因此,K4和K2被认为是最均质的单元,以浅滩环境的颗粒支撑相为主,高盐溶解的强烈影响,压实和胶结的影响较小。K3和K1单元由于相变化和成岩蚀变(白云石化作用、胶结作用和压实作用)的共同作用,表现出高度的非均质性。最后,讨论了所有储层单元的储层非均质性层序地层格架,并可作为波斯湾和中东二叠纪-三叠纪层序正在进行的储层研究的基础。

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