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Inversion for tilted triaxial conductivity in dipping layered formations

机译:倾斜层状地层中倾斜三轴电导率的反演

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摘要

In this paper, a one-dimensional inversion method is presented to determine tilted triaxial conductivity in a dipping layered formation using triaxial induction measurements. The tilted triaxial conductivity is described by three conductivity components and three Euler angles. The inversion problem is solved with the Gauss-Newton method combined with the multiplicative regularization technique. There are six principal coordinate systems that can give the same conductivity tensor. Permutation is performed to eliminate the ambiguity of inversion results caused by the ambiguity of the principal coordinate system. Three new Euler angles after permutation for each layer can be found by solving a nonlinear equation.
机译:在本文中,提出了一种一维反演方法,使用三轴感应测量来确定浸渍层中倾斜的三轴电导率。倾斜的三轴电导率由三个电导率分量和三个欧拉角描述。高斯-牛顿法结合乘法正则化技术解决了反演问题。有六个可以给出相同电导率张量的主坐标系。执行置换以消除由主坐标系的歧义引起的反演结果的歧义。通过求解非线性方程,可以找到每个层置换后的三个新的欧拉角。

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