首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Prestack depth migration of primary and surface-related multiple reflections: Part II - Identification and removal of residual multiples
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Prestack depth migration of primary and surface-related multiple reflections: Part II - Identification and removal of residual multiples

机译:一次和与表面相关的多次反射的叠前深度偏移:第二部分-识别和去除残余多次波

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摘要

Depth imaging using primary and multiple reflections (DIPMR), as described in Part I of this study, allows subsurface information carried by multiple reflections to be utilized. In the presence of strong lateral heterogeneity, however, the migration results may be distorted by artifacts originating from reflections associated with layers above the imaging plane that are commonly referred to as crosstalk. We present an image enhancement procedure that allows such artifacts to be effectively suppressed by predicting the initial crosstalk in a second migration phase. This second migration uses reflections imaged at shallower depth levels and requires knowledge of the total and primary downgoing wavefield at the receiver level. The predicted crosstalk image itself may assist the interpretational effort by indicating areas where artifacts may result in incorrect identification of geologic structures or may cause local distortions of amplitude information. Furthermore, a clean depth image can be obtained by adaptively subtracting the predicted crosstalk-related noise from the original image. The proposed method is an extension of the DIPMR procedure outlined in Part I of this study. However, it is also applicable to seismic data imaged by using conventional migration techniques that are based exclusively on primary reflections. In the latter case, the enhancement procedure allows the effects of imperfect multiple removal during preprocessing to be revealed in the migrated sections. When applied to synthetic data simulated for a complex salt model, the proposed enhancement procedure proved to be valid and effective.
机译:如本研究的第一部分所述,使用一次反射和多次反射(DIPMR)进行深度成像可以利用多次反射携带的地下信息。但是,在存在强烈的横向异质性的情况下,迁移结果可能会因伪影而失真,这些伪影源自与成像平面上方的层相关联的反射(通常称为串扰)。我们提出了一种图像增强程序,可以通过预测第二个迁移阶段的初始串扰来有效抑制此类伪像。第二次迁移使用在较浅的深度级别成像的反射,并且需要了解接收器级别的总和主要下行波场。预测的串扰图像本身可以通过指示伪影可能会导致对地质结构的错误识别或可能导致幅度信息局部变形的区域来辅助解释工作。此外,可以通过自适应地从原始图像中减去预测的与串扰相关的噪声来获得干净的深度图像。提出的方法是本研究第一部分中概述的DIPMR程序的扩展。但是,它也适用于通过使用仅基于一次反射的常规偏移技术成像的地震数据。在后一种情况下,增强过程允许在迁移过程中揭示预处理过程中不完全多次去除的效果。当应用于复杂盐模型模拟的合成数据时,所提出的增强程序被证明是有效和有效的。

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