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Determination of Structural Dip and Azimuth from LWD Azimuthal Propagation Resistivity Measurements in Anisotropic Formations

机译:在各向异性地层中的LWD方位角传播电阻率测量确定结构浸和方位角的确定

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With the use of both azimuthal propagation resistivity main and cross component data, the resistivity anisotropy and its dip and azimuth angles of a massive formation (anisotropic shale or laminated sand) can be determined. The accuracy of the determined parameters depends on the amount of available data. A minimum amount of data are two frequency main components and real and quadrature cross components. The boundary effects will distort the solution eventually; however, the anisotropy enhanced processing will minimize the effects to extend the algorithm to a certain distance away from a boundary.
机译:随着方位传播电阻率的主要和交叉分量数据,可以确定电阻率各向异性及其浸入大规模形成(各向异性页岩或层压砂)的电阻率各向异性及其倾角和方位角。所确定的参数的准确性取决于可用数据的量。最小数量的数据是两个频率的主要组件和真实和正交交叉组件。边界效应最终会扭曲解决方案;然而,各向异性增强的处理将使效果最小化将算法扩展到远离边界的一定距离。

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