储层建模使用薄层分析和表征e-tlac™方法浊积岩环境

G. Gangemi, M. Galli, F. Cruciani, G. Barbacini, M. Dallorto
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引用次数: 0

摘要

薄浊度硅质储层是一个具有挑战性的深水环境。在西非的一个深海近海油田,这些储层的沉积学特征表明是典型的浊积砂岩:砂砾岩具有中等粒度和正常级配,由泥质层插入的平面平行砂层叠加(晚期浊积砂岩层- Mutti, 1992年的特征)。含油油藏既产厚层砂,也产薄层砂。据推测,高达40%的砂页岩层间层厚度小于0.3m。在储层模型中,通过岩石物性曲线、测井相曲线、薄层层段特征曲线和地震反演量来定义这些砂岩。调谐分析表明,潜在的地震分辨率为16米。对地震反演进行处理,生成更高分辨率的建模驱动。地层评价使用“薄层分析和表征”(e-tlac™)方法(Galli等人,2002年)中的高分辨率测井资料,该方法有助于增强薄层间相表征,而常规测井资料无法捕获这些特征。该方法提供了用薄岩性工具测井的含砂量、孔隙度和饱和度的估计。在该油田的12口井中,只有3口井获得了高分辨率测井数据。因此,需要重新校准所有常规cpi,包括“e-tlac”输出结果,以更好地控制整个电网的储层物性分布。该方法提高了储层体积估算能力,使其更接近真实值,避免了净含砂饱和度的低估和含水饱和度的高估。在静态3D模型中建立薄浊积砂岩模型的解决方案是整合上述所有数据输入(地层环境、地震反演体积和“e-tlac”输出)。储层岩心是沉积学研究的输入;地震反演量是储层相分布和“e-tlac™”地层评价输出的背景资料,用于将储层属性无偏地分配给井位的砂层和薄层相。根据经验教训,获取三轴感应、高分辨率电介质或图像是更好地表征类似深水环境中存在的层间薄层的关键。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Reservoir Modeling using Thin Layer Analysis and Characterization e-tlac™ Approach for Turbiditic Environment
Thin turbidity siliciclastic reservoir is a challenging deep-water environment for modeling. In a deep off-shore field in West Africa, sedimentological characterization of these reservoir suggests typical turbiditic sandstones: Arenites with medium granulometry and normal gradation over imposed by plane-parallel sand laminations intercalated by shaly levels (late stage turbidity sandstone beds - characterization by Mutti, 1992). The oil bearing reservoir, is producing both from thick sands and thin layer sands. It is supposed the presence of up to 40% of sand-shale inter-bedded layers with a thickness less than 0.3m. These sands are defined in the reservoir model by curves of petrophysical properties, log facies, characterization of thin bedded intervals and a volume of seismic inversion. Tuning analysis suggest the potential seismic resolution is 16 meters. Seismic inversion was processed to generate a higher resolution driver for modelling. Formation evaluation uses high-resolution logs within "Thin Layer Analysis and Characterization" (e-tlac™) method (Galli et Al., 2002) which helps enhancing thin inter-bedded facies characterization, not captured with conventional logs. The method provides an estimate of the Sand content, Porosity and Saturation logged by the tools with thin lithology. High-resolution logs were acquired only in three wells over twelve drilled in the field. For this reason, a re-calibration of all conventional CPIs including the "e-tlac" output results was necessary to better control the reservoir property distribution all over the grid. This methodology increased capability estimating pay volume close to real value avoiding underestimation of Net Sand and Water Saturation overestimation. The solution to model thin turbiditic sands within the static 3D model is integrating all the above data inputs (stratigraphical environment, seismic inversion volume and "e-tlac" output). Reservoir cores was the input for the sedimentological study; the seismic inversion volume was background for reservoir facies distribution and "e-tlac™" formation evaluation output to assign unbiased reservoir properties to sand and thin layer facies at the well position. As lesson learned, the acquisition of triaxial induction, high-resolution dielectric or image is the key to better characterize the inter-bedded thin levels that are present in similar deep-water environment.
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