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Prediction of the s-wave velocity in carbonate formation using joint inversion of conventional well logs

机译:利用常规测井联合反演预测碳酸盐岩中的s波速度

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In this paper, we propose a technique for the prediction of s-wave velocity in carbonate formations with different types of secondary porosity using conventional logs (p-wave slowness, micro-resistivity, total porosity and density). The technique consists of the determination of the pore microstructure parameters ( matrix and secondary porosities, shapes of the secondary pores) using the joint petrophysical inversion of well logs and simulation of the s-wave log for the medium with obtained characteristics. In the inversion procedure, the calculation of the theoretical logs is based on the model of a double-porosity medium that consists of a homogeneous isotropic matrix with a primary pore system and secondary pores approximated by spheroidal inclusions placed in the matrix. Selecting the aspect ratio of inclusions we have simulated different types of secondary porosity such as vugs ( close to spherical inclusions), vugs connected by channels ( prolate spheroids) and cracks ( flattened spheroids). We have applied the self-consistent method ( the effective medium approximation) to simulate physical properties including the s-wave slowness from the double-porosity model. The technique has been verified using a theoretical model and experimental data from the South Zone of Mexico. The results of this technique application have demonstrated a good agreement between measured and reconstructed s-wave logs in carbonate formations.
机译:在本文中,我们提出了一种使用常规测井(p波慢度,微电阻率,总孔隙度和密度)来预测具有不同类型次生孔隙度的碳酸盐岩地层s波速度的技术。该技术包括使用测井联合岩石物理反演确定孔隙微结构参数(基质和次要孔隙度,次要孔隙的形状)以及模拟具有所获得特征的介质的s波测井。在反演过程中,理论测井的计算是基于双孔隙介质的模型,该模型由均质各向同性的基体组成,该基体具有一个初级孔隙系统和一个次级孔隙,该次级孔隙由放置在该基质中的球形夹杂物近似。选择夹杂物的长宽比,我们已经模拟了不同类型的次生孔隙度,例如孔洞(接近球形夹杂物),通过通道连接的孔洞(长椭球形)和裂缝(扁平球状)。我们已经应用了自洽方法(有效介质近似)来模拟物理性质,包括双孔隙率模型中的s波慢度。该技术已使用来自墨西哥南部地区的理论模型和实验数据进行了验证。该技术应用的结果表明,碳酸盐岩地层中实测和重建的s波测井曲线吻合良好。

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