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Theory of interval traveltime parameter estimation in layered anisotropic media

机译:层状各向异性介质中间隔传播时间参数估计的理论

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Moveout approximations for reflection traveltimes are typically based on a truncated Taylor expansion of traveltime squared around the zero offset. The fourth-order Taylor expansion involves normal moveout velocities and quartic coefficients. We have derived general expressions for layer-stripping second-and fourth-order parameters in horizontally layered anisotropic strata and specified them for two important cases: horizontally stacked aligned orthorhombic layers and azimuthally rotated orthorhombic layers. In the first of these cases, the formula involving the out-of-symmetry-plane quartic coefficients has a simple functional form and possesses some similarity to the previously known formulas corresponding to the 2D in-symmetry-plane counterparts in vertically transversely isotropic (VTI) media. The error of approximating effective parameters by using approximate VTI formulas can be significant in comparison with the exact formulas that we have derived. We have proposed a framework for deriving Dix-type inversion formulas for interval parameter estimation from traveltime expansion coefficients in the general case and in the specific case of aligned orthorhombic layers. The averaging formulas for calculation of effective parameters and the layer-stripping formulas for interval parameter estimation are readily applicable to 3D seismic reflection processing in layered anisotropic media.
机译:反射行程时间的时差近似值通常基于行程时间的截断泰勒展开,该展开次数围绕零偏移量平方。四阶泰勒展开涉及正常的运动速度和四次系数。我们导出了水平分层各向异性地层中剥离二阶和四阶参数的一般表达式,并针对两种重要情况指定了它们:水平堆叠排列的正交斜交层和方位旋转的正交斜交层。在这些情况中的第一种情况下,包含不对称平面四次系数的公式具有简单的函数形式,并且与对应于垂直横观各向同性(VTI)的2D不对称平面对应项的先前已知公式具有某些相似性)媒体。与我们得出的精确公式相比,使用近似VTI公式近似有效参数的误差可能会很大。我们已经提出了一个框架,该框架用于在一般情况下和正交各向异性层的特定情况下从行程时间扩展系数推导间隔参数估计的Dix型反演公式。用于计算有效参数的平均公式和用于间隔参数估计的层剥离公式很容易适用于分层各向异性介质中的3D地震反射处理。

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