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

H. Zakaria, M. Al-Hammadi, C. Lehmann, Sultan Dahi Al-Hassani, S. Ahmed, O. Khan, A. Al-Ali
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Abstract

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.
海上中侏罗统储层成岩作用及储层物性的相控制识别
为了了解储层质量和储层构型,对海上中侏罗统储层进行了沉积学研究。内部岩心描述、裸眼岩石物理测井解释和常规岩心分析分析,使作者能够解释沉积环境,并绘制手绘相图,以了解相结构;根据沉积环境和成岩作用的不同,形成相格局。在整个油田的18口井中,共描述了2285英尺的岩心和1799个薄片。岩心的描述以1:50的比例完成,整个油藏剖面拍摄了约495个薄片。详细描述了结构和动物含量,以及沉积特征,以确定沉积模式和相结构。通过对成岩特征和孔隙类型的分析,得出了储层质量控制因素。综合考虑这些因素,建立了既能反映沉积环境又能反映成岩作用影响的相方案。在一个巨大的碳酸盐岩台地上解释了一个低起伏、非常活跃的浅滩系统。结合沉积环境和成岩作用,将不同岩相划分为5个相组。利用该模型绘制了4张手绘相图,分别代表储层X和高渗透层X7,总体趋势为油田北部较好相。这项工作的新颖之处在于,由于大量的棘皮动物导致胶结程度的差异,从而降低了储层的质量,识别出这些主要的棘皮动物相带,可以帮助我们更好地布置井。
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