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Chemical Compaction as the Driving Mechanism for Reservoir Quality Variation in an Early Cretaceous Middle Eastern Carbonate Reservoir

机译:化学压实作为早期白垩纪中东碳酸盐储层储层水库质量变异的驱动机制

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Reservoir 2 shows the same vertical facies stacking pattern across Oilfield A.These facies are observed to be laterally continuous across other oilfields in Abu Dhabi.Multi-scale static and dynamic data show a north to south degradation in reservoir quality across the field.A petrographic,core and borehole imagebased evaluation has generated a robust geological concept governing porosity and permeability distribution across Reservoir 2 that is calibrated to seismic impedance and dynamic data.Diagenetic phases were quantified and mapped as part of a detailed sedimentological and petrographic description of Reservoir 2.Samples were analysed for stable isotopes and fluid inclusion microscopy.Chemical compaction features were described in detail in high quality cores.The cored intervals feature abundant preserved samples with up to 30% of the cored interval unavailable for reservoir characterization due to preservation.Consequently,a detailed borehole image description was undertaken and utilized to describe the structural features at log scale and fill in the missing core sample gaps.Petrographic description and mapping shows calcite cement occludes almost all macroporosity in the south of Reservoir 2.The abundance of cement decreases towards the north.Core and BHI based descriptions of chemical compaction features show a higher abundance of stylolites in the south Reservoir 2 than in the north.Most of the primary fluid inclusions trapped within calcite cements are monophase,potential evidence that pore-filling calcite started to precipitate under cooler burial conditions,at temperatures between 60-70°C.It is proposed that stylolitisation is contemporaneous with cementation where carbonate material dissolved during chemical compaction formed the main source for cement precipitation.Reservoir 2 is up to 10% thinner in the south of Oilfield A than in the north.Increased chemical compaction in the south is correlated with decreased reservoir thickness.There is a strong correlation between the pattern of reservoir thickness and P-impedance from seismic inversion.P-impedance is negatively correlated to porosity.Stylolites are most common in reservoir intervals 2A and 2B.These intervals display a wide range of porosity and permeability from north to south,while in contrast reservoir interval 2C,with very few stylolites,has a narrow range of porosity and permeability variation field wide.It is proposed that chemical compaction is the key driver for degrading reservoir quality in Reservoir 2.All scales of static and dynamic data have been reconciled to show that chemical compaction,cementation and reservoir quality are intimately related processes.The implications for producer and injector well design are significant.Depending on the location of the planned well and the development interval to be drilled,well spacing and reservoir contact should vary accordingly,while maintaining the optimal field development pattern.
机译:储存器2显示了跨油田堆叠图案的相同垂直相位。观察到这些相块在阿布扎比的其他油田中被观察到横向连续。静态静态和动态数据显示北方的储层质量的南部南部。岩石,核心和钻孔图像被淘汰的评估产生了一种稳健的地质概念,用于储存器2的孔隙率和渗透性分布,储存器2被校准以抗震阻抗和动态数据量化阶段被定量和映射为储层的详细沉积和岩石图的一部分.Samples分析了稳定同位素和流体包容性显微镜。在高质量的核心中详细描述了化学压实特征。芯片间隔具有丰富的保存样本,该样本高达30%的芯片间隔,因保存而无法进行储层表征.Consequally,详细钻孔图像描述并进行了倾斜描述日志规模的结构特征,并填写缺失的核心样本空白。预知描述和映射显示方解石水泥遮挡几乎所有储层南部的宏观度。水泥的丰度朝向北部的水泥减少化学压实特征在南储层2中显示出比北方的曲柄高的丰度高于北部。陷入方解石水泥内的主要液体夹杂物是单相中,孔填充方解石在温度下在冷却器埋葬条件下开始沉淀出来的潜在证据。提出了60-70°C的介于在化学压实期间溶解的碳酸酯材料形成的碳酸盐溶解形成的水泥沉淀的主要来源。油田A的南部比北方的南部高达10%较薄。南方的化学压实增加与储层厚度下降相关。很强大的有限公司储层厚度模式与来自地震反转的P抗性之间的Rrelation与孔隙率呈负相关.Stylites在储层间隔2a和2b中最常见。这些间隔显示出从北到南部的各种孔隙率和渗透率。虽然在对比度储层间隔2c中,具有很少的曲柄,但具有窄范围的孔隙率和渗透性变化场。提出了化学压实是用于储存器中的储层质量的钥匙驾驶员2.静态和动态数据的所有尺度具有一直和解化学压实,胶粘剂和储层质量是密切相关的过程。对生产者和喷射器的影响很重要。在计划井的位置和钻井的发展间隔,井间距和储层应联系。应该相应地,同时保持最佳场开发模式。

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