南海东部海域砂岩粒度的电成像响应特征分析

    Formation micro-imaging response characteristics of sandstones with different grain sizes in the eastern South China Sea

    • 摘要: 南海东部海域砂岩储层的高效勘探开发亟须明确不同粒度砂岩的电成像测井(FMI)响应特征,以解决常规测井方法在有效区分中砂岩、细砂岩、粉砂岩和泥岩方面存在的困难,为储层孔隙结构定量评价提供依据。以恩平地区A井为主要研究对象,选取中砂岩、细砂岩、粉砂岩和泥岩的典型层段,系统统计其电成像微电阻率数据,通过计算平均电阻率、标准差和变异系数,结合泥质含量与孔隙度参数开展特征关联性分析,建立了岩性分类图版与孔隙度预测模型。结果表明,不同岩性的电成像响应特征表现出良好的区分能力:平均电阻率数值从中砂岩、细砂岩、粉砂岩到泥岩依次递减;图像非均质性差异明显,粉砂岩与泥岩的变异系数显著高于中砂岩与细砂岩,与FMI图像中观察到的斑驳纹理特征相吻合。基于此,本研究创新性地建立了综合岩性分类图版,同时建立了孔隙度与平均电阻率、变异系数的多元统计模型,其拟合度达0.837,实现了基于电成像宏观图像特征的岩性分类与孔隙度半定量预测方法。研究明确了不同粒度砂岩的电成像响应特征规律,建立的岩性分类与孔隙度预测方法有效解决了常规测井岩性区分难题,为南海东部海域砂岩储层评价提供了可靠技术参考。

       

      Abstract: To achieve efficient exploration and development of sandstone reservoirs in the eastern South China Sea, there is an urgent need to determine the formation micro-imaging (FMI) response characteristics of sandstones with different grain sizes. This effort will help overcome the limitations of conventional logging methods in distinguishing medium-grained sandstones, fine-grained sandstones, siltstones, and mudstones, thereby providing a basis for the quantitative evaluation of reservoir pore structures. This study investigated typical intervals of medium-grained sandstones, fine-grained sandstones, siltstones, and mudstones in well A in the Enping area. Specifically, a systematic statistical analysis was conducted for the FMI data of these rocks. By calculating the average resistivity, standard deviation, and coefficient of variation (CV) and combining shale content and porosity parameters, this study conducted a correlation analysis of the FMI response characteristics. Accordingly, a chart board for lithology classification and a porosity prediction model were established. The results show that different rocks exhibited distinct FMI response characteristics. The average resistivity of various sandstones decreased in the order of medium-grained sandstones, fine-grained sandstones, siltstones, and mudstones, with image heterogeneity differing significantly. The siltstones and mudstones exhibited markedly higher CV values than medium- and fine-grained sandstones, aligning with the mottled texture observed in FMI images. Based on these findings, a comprehensive chart board for lithology classification was innovatively developed. Furthermore, a multivariate statistical model relating porosity to average resistivity and CV was created, achieving a goodness-of-fit of 0.837. Therefore, methods for lithology classification and semi-quantitative porosity prediction based on macroscopic FMI characteristics were achieved. Overall, this study clarifies the patterns of FMI responses of sandstones with different grain sizes, and the proposed methods for lithology classification and porosity prediction can effectively address the challenge of lithology differentiation using conventional logging. The results of this study provide a reliable technical reference for the evaluation of sandstone reservoirs in the eastern South China Sea.

       

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