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CHARACTERIZATION OF CARBONATE FORMATIONS USING THE JOINT INVERSIóN OF CONVENTIONAL WELL LOGS

机译:常规井原木联合inversión的碳酸盐醛形成的表征

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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, total 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 the shale concentration, dolomite concentration, 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 others 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:在本文中,我们提出了一种新方法,用于确定含有Halales双孔隙碳酸酯形成的岩性和岩石物理特征的新方法。该方法基于岩石物理性质的理论计算和以下常规日志的关节同时反演:P-和S波分流时间,电阻率,密度,总孔隙率和伽马射线。反转过程在最小化包括测量和计算的日志之间的加权方差和的成本函数,以及包含附加信息的正则化功能(其变体的初始模型参数和范围)。由反转确定的岩石物理参数是页岩浓度,白云石浓度,基质孔隙率,二次孔隙率和次级孔隙率(近似次级孔隙的纵横比)。为了计算理论日志,我们使用对应于由横向各向同性介质组成的形成模型,该介质由不同类型和Shales的二级孔隙率构成的晶体层。碳酸盐岩被视为复合材料,其由均相各向同性基质(固体骨架和基质孔系统)组成,其中嵌入由球状体表示的二次孔。考虑到固体组分的矿物成分来计算基质物理性质。为了计算有效属性,我们应用有效媒体近似的对称自我一致方法。页岩属性也可以考虑其他矿物和流体特性,通过对每个日志的误差分布的后析分析进行调整。从墨西哥南部区域的vuggy和骨质碳酸盐储存器的各种钻孔的联合反演结果表现出与核心数据,图像日志和地质描述的良好对应关系。基于实验数据,我们证明了输出反演参数可用于改善碳酸盐型硅酸盐分类和渗透预测所需的次孔互连的分类。

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