综合钻孔图像分析在改进地质模型中的价值——以科威特Greater Burgan油田为例

B. Al-Enezi, B. Kostic, Nicola Foote, J. Filak, F. Al-Mahmeed, O. Al-Shammari, M. Bertouche
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引用次数: 0

摘要

电阻率成像测井是一种高分辨率的工具,可以帮助解开井筒中的沉积和构造组织。当对岩心进行校准时,它们提供了一个特别强大的数据集,最大限度地提高了它们对油藏特征的益处。本文展示了从Greater Burgan油田选定井中进行的非常详细的图像评估如何帮助约束白垩纪Burgan和Wara储层的地层模型和沉积解释。一项针对123口取心井的多学科研究,整合了岩心沉积学、岩石学、生物和化学地层学、电缆井和电阻率成像测井,为世界上最大的硅屑油田中最重要的储层之一提供了一个强大的地层和沉积框架。根据岩心和常规测井资料校准的描述性图像相方案可以捕获储层的岩性变化、沉积特征和表面,为未取心层段和井的沉积学评估提供详细的替代方案。富砂的布尔干下部(4S)由细粒至极粗粒的河道砂体组成,这些砂体局部被侧向受限的泥岩挡板隔开。图像和岩心分析表明,大部分砂岩为高角度交错层状,在混合河道砂体内形成堆积状条形。它们一致的NE-E方向支持低曲度(辫状)河流体系,导致整个油田形成相对简单的片状沉积体系。布尔干河中部取心砂体(3SM)虽然粒度稍细,但与布尔干河下游砂体相似。然而,成像井的古流体数据显示,砂质barform的方向分布较大,约为c - 60°-90°,主要为N - E方向。仔细分析砂岩包体之间的边界面方向可以发现,在一些井中,倾斜取向和大致平行的取向比例几乎相等。这表明至少有一些侧向(点)坝的形成,并且可能存在更高弯曲度的河道,这意味着相对于布尔干下部,布尔干中部的砂体结构和流体流动路径可能更为复杂。Burgan和Wara地层的例子突出了集成图像分析对储层特征的价值,通过提供一致的描述框架,嵌入不同的数据集。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Value of Integrated Borehole Image Analysis to Refine Geological Models: An Example From the Greater Burgan Field, Kuwait
Resistivity image logs are high-resolution tools that can help to unravel the depositional and structural organisation in a wellbore. They provide a particularly powerful dataset when calibrated against core, maximising their benefit for reservoir characterisation. This paper shows examples how very detailed image assessment from selected wells in the Greater Burgan Field has helped to constrain the stratigraphic model and depositional interpretations of the Cretaceous Burgan and Wara reservoirs. A multidisciplinary study of 123 cored wells, integrating core sedimentology, petrography, bio- and chemostratigraphy, wireline well and resistivity image logs, has delivered a robust stratigraphic and depositional framework for one of the most important reservoirs in the world's largest siliciclastic oil field. A descriptive image facies scheme that has been calibrated against core and conventional well logs captures the lithological variation, sedimentary features and surfaces of the reservoir, providing a detailed proxy for the sedimentological evaluation of uncored intervals and wells. The sand-rich lower Burgan (4S) comprises fine to very coarse-grained fluvial channel sandbodies that are locally separated by laterally restricted mudrock baffles. Image and core analyses suggest that the majority of the sandstones are high-angle cross-stratified and form stacked barforms within amalgamated channel sandbodies. Their consistent orientation towards the NE-E supports a low-sinuosity (braided) fluvial system resulting in a relatively simple, sheet-like depositional architecture across the field. Although slightly finer grained, the cored middle Burgan channel sandbodies (3SM) are similar to those in the lower Burgan. However, palaeoflow data from the imaged wells show a higher directional spread in the order of c.60-90° with a dominantly N to E orientation of the sandy barforms. Careful analysis of the orientation of the bounding surfaces between the sandstone packages indicates nearly equal proportions of obliquely and roughly parallel dip orientations in some wells. This suggests the formation of at least some lateral (point) bars and possibly the presence of higher sinuosity channels implying that sandbody architecture and fluid flow pathways could be more complex in the middle Burgan relative to the lower Burgan. The examples from the Burgan and Wara Formations highlight the value of integrated image analysis for reservoir characterisation by delivering a consistent descriptive framework, embedding different datasets.
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