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Seismic Characterization of the Shuaiba Formation in the Western Region of UAE, a Predictive Tool to unravel Shuaiba Facies Mosaic?

机译:阿联酋西部地区舒河地区的地震表征,一种预测舒亚比亚马赛克的预测工具吗?

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The Aptian Shuaiba Formation is among the most important reservoir units in the Middle East. Despite being extensively studied in recent years (Droste, 2016; Murris, 1980; Droste and van Steenwinkel, 2004; Yose et al., 2006; 2010; van Buchem et al., 2002, 2010; Vahrenkamp, 1996), the interpretation of the Shuaiba depositional geometries, and specifically those associated with Shuaiba reservoirs, remains challenging in the seismic realm due to their intrinsic heterogeneity, variability and limited thickness. An integrated and iterative analysis including regional geology, well and seismic data was conducted to unravel the internal depositional geometries and associated reservoir properties for the Shuaiba Formation in the western region of UAE. In the study area, spatial distribution and geometry of the Shuaiba seismic facies was mapped in detail using full-stack reflectivity, discontinuity, curvature and spectral decomposition seismic attributes and further integrated with available well data and analogues. The Shuaiba Formation is expressed on seismic by mounded facies characterized by an irregular appearance, with discontinuous outline of sub-transparent reflectors, crossing reflectors and a larger thickness than the surrounding facies. Reflectors may locally coalesce and form mounded features up to 70 ms thick. The areas between mounds are characterised by sub-parallel to inclined reflections. The latter could be interpreted as clinoforms, prograding from the isolated nucleation areas to their deeper surroundings. The base of the mounds is located just above the top Thamama B/base Shuaiba reflector and the top coincides with the top Shuaiba. Well data suggest that these mounds consist usually of Bacinella/Lithocodium facies and rudists. The detailed 3D seismic interpretation of the Shuaiba reservoir geometries indicates a complex depositional architecture, which results in a variety of potential stratigraphic trap geometries and a heterogeneous reservoir property distribution. The proposed integrated workflow can therefore be used as a predictive tool to unravel further prospectivity in the Shuaiba Formation and in similar complex carbonate reservoirs, as well as to significantly improve reservoir property distribution prediction in static models.
机译:Aptian Shuaiba形成是中东最重要的水库单位之一。尽管近年来广泛研究(Droste,2016; Murris,1980; Droste和Van Steenwinkel,2004; Yose等,2006; 2010; Van Buchem等,2002,2010; Vahrenkamp,1996),解释由于其内在的异质性,可变性和有限的厚度,舒巴巴沉积几何形状,特别是与水库储存器相关的人在地震领域仍然具有挑战性。进行了包括区域地质,良好和地震数据的综合和迭代分析,以解开内部沉积几何形状的内部沉积几何形状和相关储层特性。在研究区域中,使用全堆叠反射率,不连续性,曲率和光谱分解地震属性并进一步与可用的井数据和类似物进行详细映射了舒邦地震相的空间分布和几何形状。 Shuaiba形成在由不规则的外观特征的混浊面上表达,其中副透明反射器的不连续轮廓,交叉反射器和比周围的面部更大的厚度。反射器可以在局部聚结,形成多达70毫秒厚的墩特征。土墩之间的区域的特征在于与倾斜的反射副平行。后者可以被解释为临床,从分离的核心区域促进到更深的环境中。土墩的底座位于顶部Thamama B / Base Shuaiba反射器中,顶部与顶部舒吉巴相一致。井数据表明,这些土墩通常由Bacinella / Lithododium相和粗鲁斯人组成。 Shuaiba储层几何形状的详细3D地震解释表示复杂的沉积架构,这导致各种潜在的地层捕集物几何形状和异质储层性质分布。因此,所提出的综合工作流程可以用作预测工具,以在舒吉巴形成和类似的复合碳酸盐储层中解开进一步的前瞻性,以及显着提高静态模型中的储层性能分布预测。

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