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Identifying Facies Control on Diagenesis and Reservoir Quality of an Offshore Mid-jurassic Reservoir

机译:识别离岸中侏罗座水库成岩作用和水库质量的相对

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A sedimentological study of an Offshore, mid-Jurassic reservoir was carried out in order to understand reservoir quality and reservoir architecture. In-house core description, and analysis of open-hole petrophysical log interpretation and conventional core analysis, enabled the authors to interpret the depositional environment and produce hand drawn facies maps to understand the facies architecture; by developing facies scheme, depending of depositional environment comingled with diagenetic process. About 2,285 ft of core and 1,799 thinsections were described from 18 wells, distributed throughout the field. Description of core was done at 1:50 scale and about 495 thinsections were pictured throughout the reservoir section. Detailed description of textural and faunal content, along with sedimentary features was carried out to determine the depositional model and facies architecture. By analyzing the diagenetic features and porosity type, Reservoir Quality controls were derived. All these elements were taken into consideration in order to build facies scheme that not only justifies the depositional environment but also incorporates the impact of diagenesis. A low relief, very active shoal system on a giant carbonate platform was interpreted. Various Lithofacies were grouped into 5 Facies associations keeping in mind depositional environment and diagenetic impact. This model was used to make 4 hand drawn facies maps representing reservoir X and High permeable layer, X7 with general tendency of better facies in the northern part of the field. The novelty of this work is the differential degree of cementation due to the abundance of echinoderms degrading the reservoir quality, and identifying these dominant echinoderm facies zones allows us better well placement by avoiding them.
机译:进行了海上,中海储层的沉积学研究,以了解水库质量和水库建筑。内部核心描述和露天岩石物理日志解释和常规核心分析的分析,使作者能够解释沉积环境,并生产手绘面部地图,以了解相框;通过开发面部方案,取决于沉积的环境,具有成岩过程。从18个孔中描述了大约2,285英尺的核心和1,799次晶片,分布在整个领域。核心的描述在1:50规模完成,在整个储层部分中描绘了大约495个θ。对纹理和群体内容的详细描述以及沉积特征进行了沉积特征,以确定沉积模型和相框。通过分析成岩特征和孔隙型,衍生储层质量控制。考虑所有这些元素,以建立不仅仅是证明沉积环境的基础,而且含有成岩作用的影响。解释了巨型碳酸盐平台上的低浮雕,非常活跃的浅滩系统。将各种锂缺失分为5个相关联,保持沉积环境和成岩效应。该模型用于制作4个手绘面图,表示储存器X和高渗透层,X7,具有更好的领域中更好的相位的趋势。这项工作的新颖性是差异的粘合程度,因为升性的储层质量有所降低,并且鉴定这些显性的棘皮形相面积可以通过避免它们来更好地放置。

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