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Joint inversion of conventional well logs for evaluation of double-porosity carbonate formations

机译:常规测井联合反演以评价双孔隙碳酸盐岩地层

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In this paper we propose a new approach of well log data interpretation for determining lithological and petrophysical characteristics of double-porosity carbonate formations containing shales.This approach is based on the theoretical calculation of rock physical properties and joint simultaneous inversion of the following conventional logs:P-and S-wave transit times,resistivity,density,neutron porosity,and gamma ray.The inversion procedure consists in minimizing a cost function that includes the sum of weighted square differences between the measured and calculated logs,and the regularization functional containing additional information(initial model parameters and ranges of their variations).The petrophysical parameters determined by the inversion are a shale volume,dolomite volume,matrix porosity,secondary porosity and secondary porosity type(aspect ratios of spheroids approximating secondary pores).To calculate the theoretical logs we use the formation model that corresponds to a transversely isotropic medium composed of intercalated layers of carbonates with secondary porosity of different types and shales.The carbonate rocks are treated as a composite material that consists of a homogeneous isotropic matrix(solid skeleton and matrix pore system)where the secondary pores represented by spheroids are embedded.The matrix physical properties are calculated taking into account the mineral composition of solid components.For computing the effective properties we apply the symmetrical self-consistent method of the effective medium approximation.The shale properties as well mineral and fluid characteristics can be considered as known and they are adjusted by the posterior analysis of error distributions for each log.The results of joint inversion obtained for various boreholes from vuggy and fractured carbonate reservoirs of the South Zone of Mexico show a good correspondence with core data,image log,and geological descriptions.Based on the experimental data we demonstrate that the output inversion parameters can be used to improve the classification of carbonate lithotypes and assessment of the secondary pore interconnections required for the permeability prediction.
机译:本文提出了一种测井资料解释的新方法,用于确定含页岩的双孔隙碳酸盐岩地层的岩性和岩石物理特征,该方法基于岩石物理性质的理论计算和以下常规测井的联合同时反演: P波和S波的传播时间,电阻率,密度,中子孔隙率和伽马射线。反演程序包括将成本函数最小化,该成本函数包括测得和计算的测井曲线之间的加权平方差之和,以及包含附加值的正则函数反演确定的岩石物理参数为页岩体积,白云石体积,基质孔隙度,次生孔隙度和次生孔隙类型(近似于次生孔隙的球体的纵横比)。日志,我们使用对应于的形成模型由各类型和页岩的次级孔隙度的碳酸盐插层组成的横向各向同性介质。碳酸盐岩被视为由均质各向同性基质(固体骨架和基质孔隙系统)组成的复合材料,其中以球体表示的次级孔隙为考虑固体成分的矿物成分来计算基体的物理性质,为计算有效性质,我们采用有效介质近似的对称自洽方法,可以将页岩性质以及矿物和流体特征视为通过对每个测井的误差分布进行后验分析,可以对它们进行调整。从墨西哥南部地区的松散和裂缝性碳酸盐岩储层获得的各种井眼的联合反演结果与岩心数据,图像测井和地质情况具有很好的对应性。描述。基于实验数据,我们进行了恶魔化trate认为输出反演参数可用于改善碳酸盐岩岩性的分类和评估渗透率预测所需的次生孔隙互连。

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