首页> 外文期刊>Journal of African Earth Sciences >Sandstone reservoir zonation using conventional core data: A case study of lower cretaceous sandstones, Orange Basin, South Africa
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Sandstone reservoir zonation using conventional core data: A case study of lower cretaceous sandstones, Orange Basin, South Africa

机译:使用常规岩心数据进行砂岩储层分区:以南非奥兰治盆地下白垩统砂岩为例

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This study outlines the different methodologies used to identify and classify different rock units in the sandstone reservoirs of the Orange Basin in South Africa into flow units. The flow units are defined on the basis of conventional core porosity and the permeability of the reservoir occurring in the fluvial and shallow marine depositional environments within the lower Cretaceous period. A total of six facies were identified from the core data, and they were corroborated with gamma ray log data. Fades A1, A2, A3, and A4 are the main reservoir units with generally fine-to medium-grained sands, which dominantly comprise quartz grains. Fades A5 mainly comprises silts with lenses of fine-grained sands, while Fades A6 is claystone laminated with minor burrows filled with shale and occasional siltstone presence. The porosity and permeability were used to compute the permeability/porosity relationship, the rock quality index, pore spaces, storage and flow capacity values, and to indicate the flow zone. The highest porosity and permeability values correspond to fades Al and A2, which are represented by mega pore spaces, and they displayed high flow capacity values and moderate to high storage capacities. The lowest porosity and permeability values belonged to core facies A6 and AS, which mostly comprise siltstone and clay with Nano pore spaces. The flow zone indicator (FZI) values determined ranges from 0.01 to 13.9 mu m, which were grouped into four different hydraulic flow units (HFUs) within the cored intervals. The defined hydraulic units do not always coincide with the facies. The Windland pore throat radius (r35) calculated that pore spaces correlated better with the Lorenz flow zone plot and fades. It is recommended that the statistically derived reservoir quality index (RQI) equation of fades A1 and A2 be used to extrapolate the RQI and FZI values for other wells in the field. It is thus recommended that dynamic data be used to validate flow units.
机译:这项研究概述了用于识别和分类南非奥兰治盆地砂岩储层中不同岩石单元为流动单元的不同方法。流动单元是根据常规岩心孔隙度和在下白垩纪时期在河流和浅海沉积环境中发生的储层渗透率定义的。从核心数据中总共识别出六个相,并用伽马射线测井数据证实了它们。衰落A1,A2,A3和A4是主要储层单元,这些储层通常具有中细粒度的沙子,这些沙子主要包含石英颗粒。 Fades A5主要由粉粒状沙粒组成的淤泥,而Fades A6是黏土,夹杂着少量页岩和偶有粉砂岩的少量洞穴。孔隙率和渗透率用于计算渗透率/孔隙率关系,岩石质量指数,孔隙空间,储层和流动能力值,并指示流动区。最高的孔隙率和渗透率值对应于衰落的Al和A2,它们以巨大的孔隙空间表示,并且显示出高的流量值和中等至高的存储容量。最低的孔隙度和渗透率值属于核心相A6和AS,主要由粉砂岩和具有纳米孔隙空间的粘土组成。确定的流区指示器(FZI)值范围为0.01到13.9μm,在有芯间隔内分为四个不同的液压流量单元(HFU)。定义的液压单元并不总是与相一致。 Windland孔喉半径(r35)计算得出,孔空间与Lorenz流区图更好地相关,并且会逐渐消失。建议使用统计推导的衰落A1和A2的储层质量指数(RQI)公式来推断现场其他井的RQI和FZI值。因此,建议使用动态数据来验证流量单位。

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