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Alternating Joint Inversion of Controlled-Source Electromagnetic and Seismic Data Using the Joint Total Variation Constraint

机译:使用联合总变化约束交替变换控制源电磁和地震数据的联合反演

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摘要

An alternating joint inversion method for controlled-source electromagnetic (CSEM) and seismic data is developed. The structural constraint is used for correlating and constraining the electromagnetic (EM) resistivity and seismic velocity parameters during the inversion. The structural coupling used is the joint total variation (JTV) constraint, which is incorporated into the objective function of the individual EM or seismic inversion to enforce the structural similarity between the resistivity and velocity. In this paper, the conventional cross-gradient constraint is not preferred as it can only be used for enforcing structural similarity for 2-D or 3-D case since it is always zero for 1-D joint inversion. The JTV constraint can be applied for 1-D joint inversion, as well as for the 2-D/3-D case, which is of a broader interest. The improved Gauss-Newton (GN) is used for minimizing the objective function and for reconstructing the subsurface resistivity and velocity. The alternating joint inversion algorithm is applied for integrating land CSEM data with cross-well seismic data for subsurface reservoir evaluation and water-oil identification. Numerical examples show that the developed joint inversion can improve the inversion results significantly over those from the separate EM or seismic inversion.
机译:提出了一种控制源电磁(CSEM)和地震数据的交替联合反演方法。在反演期间,结构约束用于关联和约束电磁(EM)电阻率和地震速度参数。使用的结构耦合是联合总变化(JTV)约束,该约束被合并到单个EM或地震反演的目标函数中,以增强电阻率和速度之间的结构相似性。在本文中,传统的交叉渐变约束不是优选的,因为它只能用于增强2-D或3-D情况下的结构相似性,因为对于1-D联合反演它始终为零。 JTV约束可以应用于一维联合反演以及2-D ​​/ 3-D情况,这引起了广泛的兴趣。改进的高斯牛顿(GN)用于最小化目标函数并重建地下电阻率和速度。应用交替联合反演算法将陆地CSEM数据与井间地震数据整合起来,用于地下储层评估和水油识别。数值算例表明,与单独的EM反演或地震反演相比,开发的联合反演可以显着改善反演结果。

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