首页> 外文期刊>Journal of Environment and Earth Science >A SPECTRAL METHOD OF LITHOFACIES DIFFERENTIATION WITHIN A HYDROCARBON RESERVIOR UNIT USING SEISMIC AND WELL DATA FROM TOMBOY FIELD NIGER DELTA
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A SPECTRAL METHOD OF LITHOFACIES DIFFERENTIATION WITHIN A HYDROCARBON RESERVIOR UNIT USING SEISMIC AND WELL DATA FROM TOMBOY FIELD NIGER DELTA

机译:汽油储层装置中岩石腐蚀装置的光谱法利用Tomboy田间尼日尔三角洲的岩土储层装置分化

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Seismic facies analysis is a key component of Seismic interpretation workflow, as much information on depositional process, environment, reservoir architecture and potential can be determined from the seismic data. This enhances the seismic visibility of subtle stratigraphic features, and prediction of new prospects for drilling due to lateral continuity of sand bodies (the hydrocarbon reservoir) deposited within the sedimentary column. This study presents the results of the application of seismic amplitude inversion and spectral decomposition to differentiate lithofacies within a thin-sand reservoir and show their lateral and vertical continuity using amplitude-derived attributes (rock properties) in the interpretation of 3D seismic and well log data from “TOMBOY” field Niger Delta. A thin-sand reservoir was delineated from lithologic log signatures within the interval 11,135.61-11,210.35ft which corresponds to the time window 2.752 - 2.768secs on the seismic data along an arbitrary line drawn to connect the six wells (01-06) in the field. Crossplot of acoustic impedance against density across the reservoir bed showed three compartments interpreted as gas filled sand, oil filled sand and shale. The interpretation was enhanced via spectral analysis by computing frequency maps of acoustic impedance, density and velocity using discrete Fourier transform (DFT) technique at top (2.752sec) of the reservoir in terms of magnitude, phase and frequency. Phase response for the three attributes (acoustic impedance, density and velocity) showed lateral continuity and discontinuity of sand lithofacies at the various well locations which were not evident on their original amplitude time slice, while frequency response showed bed thickness, with low frequency indicating presence of hydrocarbon or sand rich beddings, while high frequency indicates thin shale beddings. It was observed that the top (2.752sec) of the reservoir for wells 02, 05, 01 and 04 showed low frequency values for the three attributes (acoustic impedance, density and velocity) which indicates potential zones for hydrocarbon production and development in the field, while wells 03 and 06 within the same time slice (2.752sec) showed a higher value in acoustic impedance frequency, density frequency and velocity frequency and suggests the presence of thin shale facies at the top (2.752sec) of the thin-sand reservoir. By defining the lateral and vertical continuity of sand facies within the reservoir bed, hydrocarbon fairways were better defined and knowledge of this can be incorporated into drilling decisions for field development. The results gave enhanced structural disposition of the reservoir bed and more insights into the variation of sand lithofacies with depth.
机译:地震相分析是地震解释工作流程的关键组成部分,关于沉积过程,环境,储层架构和潜力的许多信息可以从地震数据确定。这提高了微妙地层特征的地震可见度,以及由于沉积柱内沉积的砂体的横向连续性而预测钻孔的新前景。本研究介绍了地震幅度反转和光谱分解的应用结果,以区分薄砂储层内的岩石缩放,并使用幅度衍生的属性(岩石属性)显示它们的横向和垂直连续性,在释放3D地震和井日志数据的解释中来自“tomboy”田间尼日尔三角洲。薄砂储存器在间隔内的岩性对数签名中描绘,该间隔11,135.61-11,210.35英尺对应于沿着绘制六个井(01-06)的任意线的地震数据上的时窗2.752-2.768SEC。 。声阻抗对储层床密度的交叉图显示了三个隔间,被解释为气体填充的沙子,填充沙子和页岩。通过在储库的顶部(2.752SEC)的离散傅里叶变换(DFT)技术在幅度,相位和频率方面,通过计算声阻抗,密度和速度的频率图来增强解释。三个属性的阶段响应(声阻抗,密度和速度)在各种井位置显示出在其原始幅度时间片上没有明显的各种阱位置的横向连续性和不连续性,而频率响应显示床厚度,则具有低频率指示存在碳氢化合物或沙子丰富的床上床上,而高频表示薄页岩寝具。观察到井02,05,01和04的储存器的顶部(2.752sec)显示了三个属性(声阻抗,密度和速度)的低频值,这表明了该领域的碳氢化合物生产和发育的潜在区域,而在同一时间片(2.752SEC)内的井03和06在声阻频,密度频率和速度频率下显示出更高的值,并表明薄砂储存器顶部(2.752sec)的薄页岩相的存在。通过定义储层床内的砂面的横向和垂直连续性,更好地定义了碳氢化合物球道,并且可以将其知识结合到钻井决策中进行现场开发。结果提高了水库床的结构配置,并更有洞察于深度砂岩岩的变化。

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