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Integrated Fracture Study using Formation Micro Imager, Stoneley Waves and Formation Evaluation Results in Carbonate Reservoir at Gulf of Suez, Egypt

机译:综合骨折研究采用地层微成像仪,Stoneley波和地层评估结果在埃及苏伊士湾的碳酸盐储层

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The carbonate reservoirs in Gulf of Suez area have complex geological structure due to the existence of fractures associated with faults. Thus, fracture characterization of this complicated area is very important to understand the reservoir behavior and hence assigning the best completion intervals for the producing wells. In this paper, we developed a workflow of integrating formation micro imager, Stoneley waves and petrophysical analysis for better fracture characterization and selecting the best perforation intervals for a producing well. This workflow is applied on well NWO-1, in the Northwest October Concession in the Gulf of Suez area over the carbonate reservoir. The well was drilled on the peak of anticlinal feature created by fault propagation fold of a normal fault that located nearby the well. The main objective was to determine the structural geology features (i.e. fractures), its orientation and the diagenetic features (i.e. vugs) using formation micro imaging tool. Also, to quantify the effectiveness of fractures as fluid conduit mainly in the carbonate reservoirs either in Thebes or Mokattam Formation via Stoneley waves derived from processing result of sonic measurement. This is combined with the petrophysical interpretation using the elemental spectral device data and other conventional open hole logs to provide a comprehensive petrophysical formation evaluation. The study reveals that the highest average fracture density is over (Layer-A & B) at the upper most interval of Thebes Formation around 2.2 fractures/ft and (Layer-C) at the bottom around 1.77 fractures/ft. These fractures were proved to be of good fluid conduit based on both Stoneley waves and the petrophysical interpretation. The two layers A and B were recommended to be tested and the DST (Drill Steam Test) results proved the higher productivity than layer C which confirms the outcome from our integrated study.
机译:在苏伊士区域海湾碳酸盐贮存器具有复杂的地质结构由于与断层有关裂缝的存在。因此,这种复杂的区域的裂缝表征是非常重要的是理解贮存行为并且因此对于生产井分配最佳完井层段。在本文中,我们开发了集成微地层成像器,斯通利波和岩石物理分析为了更好的裂缝表征和选择最佳穿孔间隔生产井的工作流程。此工作流是在苏伊士湾面积超过所述碳酸盐岩储层施加在井NWO-1,在西北十月特许。该井钻出通过故障传播创建褶皱正断层使得位于附近阱的背斜特征的峰。的主要目的是,以确定构造地质特征(即骨折),其取向和成岩特征(即孔洞),使用形成显微成像工具。此外,为了通过从声波测量的处理结果得到的斯通利波任一量化骨折作为流体导管的有效性主要在碳酸盐岩储层中底比斯或Mokattam形成。这是通过使用所述元素光谱设备的数据和其它常规裸眼井测井提供了全面的岩石物理地层评价的岩石物理解释相结合。该研究表明,最高平均断裂密度超过(层-A&B)在约2.2骨折/英尺在底部周围1.77骨折/英尺最上面的间隔形成底比斯的和(层C)。这些裂缝被证明是基于两个斯通利波和岩石物理解释是良好的流体管道。被推荐两个层A和B被测试和DST(钻蒸汽试验)的结果证明比层C具有较高的生产率这证实我们的研究整合的结果。

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