A Workflow to Integrate Core and Image Logs in Order to Enhance the Characterization of Subsurface Facies on Carbonate Reservoirs, Offshore Abu Dhabi

E. BinAbadat, H. Bu-Hindi, C. Lehmann, Atul Kumar, H. Al-Harbi, A. Al-Ali, Adel Al Katheeri
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Abstract

In this study, core and log data were integrated to identify intervals which are rich in stromatoporoids in an Upper Jurassic carbonate reservoir of an offshore green field Abu Dhabi. The main objective of this study was to recognize and stromatoporoids floatstones/rudstones in core, and develop criteria and workflow to identify them in uncored wells using borehole images. The following workflow was used during this study: i) Identification of the stromatoporoid feature in pilot wells with core and borehole images, ii) Investigate the properties and architecture of stromatoporoid bodies, iii) Integrate the same scale of core observations with borehole images and conventional log data (gamma ray, neutron porosity and bulk density logs) to identify stromatoporoid-rich layers, iv) Performing a blind test on a well by using the criteria developed from previous steps to identify "stromatoporoid accumulations" on a borehole image, and validate it with core observations. In the reservoir under investgation, stromatoporoid floatstones/rudstones intervals were identified and recognized both on core and borehole image in the pilot wells. These distinct reservoir bodies of stromatoporoids commonly occur in upper part of the reservoir and can reach to a thickness of around 20ft. The distribution and thickness of stromatoporoid bodies as well as growth forms (massive versus branching) were recognized on core and borehole images. The accumulations varied between massive beds of containing large pieces of stromatoporoids and grainstone beds rich in stromatoporoid debris. The massive beds of stromatoporoid accumulations are well developed in the northern part of the field. These layers can enhance the reservoir quality because of their distinct vuggy porosity and permeability that can reach up to several hundred of milidarcies (mD). Therefore, it is important to capture stromatoporoid layers both vertically and laterally in the static and dynamic model. Integrating borehole image data with core data and developing a workflow to identify stromatoporoid intervals in uncored wells is crucial to our subsurface understanding and will help to understand reservoir performance. Integration of image log data which is calibrated to core and log data proved to be critical in generating reservoir facies maps and correlations, which were integrated into a sequence stratigraphic framework as well. The results were used in the static model in distribution of high permeability layers related to the distribution of stromatoporoids.
阿布扎比海上,一种整合岩心和图像测井的工作流程,以增强对碳酸盐岩储层地下相的表征
在这项研究中,综合了岩心和测井资料,确定了阿布扎比海上绿地上侏罗统碳酸盐岩储层中富含层孔虫的层段。本研究的主要目的是识别岩心中的浮岩/基岩,并制定标准和工作流程,利用井眼图像识别裸眼井中的浮岩/基岩。本研究使用了以下工作流程:i)利用岩心和井眼图像识别试验井中的叠孔体特征;ii)研究叠孔体的性质和结构;iii)将相同尺度的岩心观测与井眼图像和常规测井数据(伽马、中子孔隙度和体积密度测井)相结合,以识别富含叠孔体的层。iv)对井进行盲测,使用之前步骤开发的标准来识别井眼图像上的“层孔虫聚集”,并通过岩心观察进行验证。在研究的储层中,通过岩心和井眼图像对叠孔状浮岩/砂岩层段进行了识别。这些独特的层孔类储集体通常出现在储层的上部,厚度可达20英尺左右。在岩心和钻孔图像上识别了层孔体的分布、厚度以及生长形式(块状和分枝状)。堆积在含有大块叠孔体的块状层和富含叠孔体碎屑的粒岩层之间存在差异。在油田北部,层孔类堆积的块状层发育良好。这些层具有独特的孔洞性孔隙度和渗透率,可达数百毫当量(mD),可以提高储层的质量。因此,在静态和动态模型中,垂直和横向捕获叠孔层是很重要的。将井眼图像数据与岩心数据相结合,并开发一套工作流程来识别未取心井中的层孔层,这对我们了解地下情况至关重要,有助于了解储层的动态。将测井图像数据整合到岩心和测井数据中被证明是生成储层相图和相关性的关键,这些相图和相关性也被整合到层序地层格架中。将所得结果应用于与叠层孔虫分布相关的高渗透层分布静态模型中。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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