中东地区碳酸盐岩类型概述

M. Dernaika, Bashar Mansour, O. Aljallad, S. Koronfol
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引用次数: 1

摘要

碳酸盐岩储层的复杂性和多样性要求在定义岩石类型时采用一致的方法。需要以岩石类型为基础的岩心数据作为油藏动态建模的输入。本文的目的是详细了解岩石分型的控制因素,并开发一种独特的岩石分型方法,适用于中东地区的碳酸盐岩储层。研究人员对来自7个不同碳酸盐岩储层的1000多个岩心桥塞进行了研究。这些桥塞是从15口井中精心挑选出来的,以代表取心层段的主要性质变化。可用的数据集包括实验室测量的氦气孔隙度、渗透率、薄片和高压压汞毛细管压力(MICP)。通过获得桥塞式x射线计算机断层扫描(CT)成像,确保样品没有诱发裂缝和其他可能影响渗透率测量的异常。在薄片显微照片上分析了岩石的结构,并根据其含量将其分为颗粒状、浑浊和混合。特别注意了成岩作用,主要是压实作用、胶结作用和溶蚀作用。孔隙度被定义为颗粒间、晶间、结晶、颗粒内或孔洞。将纹理信息绘制在孔隙度-渗透率(孔隙-孔隙)域中,并确定了三种不同的孔隙-孔隙关系。每一种质地都提供了独特的烫发趋势。岩石类型根据孔隙—透岩趋势确定,并与成岩作用和毛细压力(Pc)密切相关。对于每一个孔隙—透岩走向,岩石类型通过详细的Dunham结构和不同程度的成岩作用来区分。详细的结构和成岩作用与孔隙-透岩数据和MICP具有较好的相关性,从而提供了可靠的岩石类型。一种新的岩石分型方法成功应用于不同的碳酸盐岩储层。不同储层的孔隙-透岩云根据结构和成岩作用划分出走向和范围。观察到共同的控制因素,可以帮助在该地区更多的储层中获得类似的数据。基于构造成岩作用的岩石类型为了解地质对流体流动和饱和度的影响提供了更多的见解。沿着取心层段导出了地质结构,为储层的渗透率和岩石类型提供了升级选择。
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Overview of Carbonate Rock Types in the Middle East
The complexity and diversity of carbonate reservoirs necessitate having a consistent approach in defining rock types. Core data on a rock-type basis are required as input for modelling reservoir performance. The objectives of this paper are to provide detailed understanding of the controlling factors in rock typing and to develop a unique rock-typing approach that can apply to carbonate reservoirs in the Middle East region. More than 1,000 core plugs were studied from seven different carbonate reservoirs. The plugs were carefully selected from 15 wells to represent the primary property variations along the cored intervals. The data set available included laboratory-measured helium porosity, gas permeability, thin-sections, and high-pressure mercury injection capillary pressure (MICP). Plug-scale X-ray computed tomography (CT) imaging was acquired to help ensure the samples were free of induced fractures and other anomalies that can affect the permeability measurements. Rock textures were analyzed in the thin-section photomicrographs and were classified based on their content as grainy, muddy, and mixed. Special attention was given to the diagenesis effects, mainly compaction, cementation, and dissolution. Porosity was defined as interparticle, intercrystalline, moldic, intraparticle, or vuggy. The texture information was plotted in the porosity-permeability (poro-perm) domain and was determined to produce three distinct poro-perm relationships. Each texture provided an unique poro-perm trend. Rock types were defined on the poro-perm trends and showed a strong link to diagenesis and capillary pressure (Pc). For each poro-perm trend, the rock types were distinguished by detailed Dunham textures and different degrees of diagenesis. The detailed textures and diagenesis were correlated reasonably well with the poro-perm data and MICP, hence providing robust rock types. A new rock-typing approach was successfully applied in different carbonate reservoirs. The poro-perm cloud from the different reservoirs was resolved into trends and ranges based on textures and diagenesis. Common controlling factors were observed, which can help produce data analogues along more reservoirs in the region. The texture-diagenesis-based rock types provided more insight into the effects of geology on fluid flow and saturation. Geological textures were derived along the cored intervals and provided upscaling options for permeability and rock types in the reservoirs.
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