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Model-based radiation pattern correction for interferometric redatuming in 4D seismic

机译:4D地震中干涉性重氮的模型辐射图案校正

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Interferometric virtual source (VS) redatuming converts surface-triggered source records into the equivalent records as if they originated from buried receiver locations by crosscorrelating downgoing waves with the corresponding upgoing waves. The theory suggests that when the receivers are surrounded by an enclosing boundary of sources, then the VS has an isotropic radiation pattern and yields an accurate response. The resultant records should determine improvement in the seismic repeatability and image quality compared with non-VS. However, in the presence of a complex near surface, an intricate shallow structure and highly variable weathering layers can severely distort the raypath, such that it produces uneven angle coverage to the buried VS. In addition, near-surface reverberations, surface multiples, and other mode-converted waves may leak into the time-gated early arrivals and further corrupt the direct wavefields. The above-mentioned issues can result in distorted radiation patterns and contaminated responses of the VS. We address these issues explicitly by spatially filtering the potentially contaminated direct wavefields using a zero-phase matched filter, such that the filtered wavefield is consistent with a model-based ideal direct P-wavefield observed at common receiver locations. This ideal reference response is computed from a homogeneous approximation to the local near-surface overburden on top of each VS. The phases of the original direct arrivals are preserved. Components associated with the reverberations and other noises can be effectively suppressed as their spatial radiation patterns deviate from that of the ideal single P-wave mode. Toward an isotropic radiation pattern by the iterative matched filter, we reduce the unbalanced illumination arising from imperfect source coverage and near-surface complexity. Compared with previous methods, the new VS approach provides significantly improved image quality and repeatability based on a pilot field o
机译:干涉测量虚拟源(VS)REDATUMING将表面触发的源记录转换为等效记录,就好像它们通过与相应的上行波串起的追溯波互连的追溯波源自掩埋接收器位置。该理论表明,当接收器被围绕源的封闭边界包围时,VS具有各向同性辐射图案,并产生准确的响应。结果记录应确定与非VS相比的地震重复性和图像质量的改善。然而,在近近表面的复杂性存在下,复杂的浅结构和高度可变的风化层可以严重扭曲雷达,使得它产生不均匀的角度覆盖范围。另外,近表面混响,表面倍数和其他模式转换波可能会泄漏到时间门控早期港口中并进一步损坏直接波场。上述问题可能导致对VS的抗扭的辐射模式和受污染的反应。我们通过使用零相位匹配的滤波器在空间上过滤可能污染的直接波场来解决这些问题,使得滤波的波场与在公共接收器位置观察到的基于模型的理想直接p波面。这种理想的参考响应是从均匀近似计算到每个与局部对的局部近表面覆盖层的近似值。保留了原始直接抵达的阶段。可以有效地抑制与混响和其他噪声相关联的组件,因为它们的空间辐射图案偏离理想单个P波模式的空间辐射图案。通过迭代匹配过滤器朝向各向同性辐射图案,我们降低了不完美的源覆盖率和近表面复杂性引起的不平衡照明。与以前的方法相比,新的VS方法基于试验领域o提供显着改善的图像质量和可重复性

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