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Crosshole seismic tomography: working solutions to issues in real data travel time inversion

机译:井间地震层析成像:实际数据传输时间反演中问题的有效解决方案

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摘要

In travel time inversion of crosshole seismic tomography, when dealing with real data, the following three issues need to be addressed: how to suppress the effect of data errors, how to balance the data contribution and reference model, and how to properly set the geological constraints ( well logs) in an inversion. Signal-to-noise ratios of travel time data picked from real crosshole seismic surveys likely depend on the vertical offset between a source and a receiver, since the overall attenuation will typically be greater for a longer ray path. Therefore, to suppress the effect of data errors in a least-squares solution, a data confidence matrix is used in practice where the weighting is set logically based on the vertical offset. When a model constraint is adopted in the inversion to seek a solution with least deviation from some prescribed background that is most likely to have no spurious structure, a trade-off parameter is used to explicitly balance the dependence of the inversion solution to the data contribution and the reference model. The latter is built by combining sonic logging information, which is hard geological evidence at the vicinity of wells, and an initial estimate from the travel time back-projection, a preliminary solution of the travel time tomography. Geological constraints are set so that the inversion solution should have the least deviation from the hard geological evidence, and more deviation for the remaining part of the survey region, since the true velocity model might differ from such an initial estimate and the true ray paths might deviate from the initial ray paths.
机译:在井间地震层析成像的旅行时间反演中,处理真实数据时,需要解决以下三个问题:如何抑制数据误差的影响,如何平衡数据贡献和参考模型以及如何正确设置地质反演中的约束条件(测井)。从真实的井间地震勘测中采集的传播时间数据的信噪比可能取决于源与接收器之间的垂直偏移,因为对于更长的射线路径,总体衰减通常会更大。因此,为了抑制最小二乘解中的数据错误的影响,在实践中使用数据置信度矩阵,其中基于垂直偏移在逻辑上设置权重。当在反演中采用模型约束以寻求与某些规定背景的偏差最小的解决方案时,最有可能没有虚假结构的情况下,权衡参数将用于明确平衡反演解决方案对数据贡献的依赖性和参考模型。后者是通过结合声波测井信息(这是井附近的坚硬地质证据),以及行程时间反投影的初步估计(行程时间层析成像的初步解决方案)而构建的。设置地质约束条件是为了使反演解决方案与硬地质证据的偏差最小,而对于勘测区域的其余部分则偏差更大,因为真实速度模型可能与这种初始估计有所不同,真实射线路径可能有所不同偏离初始光线路径。

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