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

机译:使用常规井测井的关节反转预测碳酸酯形成中的S波速度

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摘要

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原木(P波缓慢,微电阻率,总孔隙率和密度)用不同类型的次级孔隙率预测碳酸盐岩中的S波速度的技术。该技术包括使用孔记录的关节岩石物理反演的孔微观结构参数(矩阵和次要孔隙率,次要孔隙的形状)组成,并且对于具有获得的特征的介质的S波日志的仿真和模拟。在反转过程中,理论原影的计算基于双孔隙培养基的模型,其由具有主孔系统的均匀各向同性基质组成,并且由放置在基质中的球形夹杂物近似的次要孔。选择夹杂物的纵横比我们已经模拟了不同类型的次要孔隙率,例如Vugs(靠近球形夹杂物),通过通道连接的Vugs(环形球体)和裂缝(扁平的球状体)。我们已经应用了自我一致的方法(有效介质近似)来模拟包括来自双孔隙率模型的S波缓慢的物理性质。该技术已经使用来自墨西哥南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,在碳酸盐形成中测量和重建的S波日志之间的良好一致性。

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