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首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Imaging internal multiples from subsalt VSP data - Examples of target-oriented interferometry
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Imaging internal multiples from subsalt VSP data - Examples of target-oriented interferometry

机译:从盐下VSP数据成像内部倍数-面向目标的干涉仪的示例

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摘要

Seismic interferometry has become a technology of growing interest for imaging borehole seismic data. We demonstrate that interferometry of internal multiples can be used to image targets above a borehole receiver array. By internal multiples, we refer to all types of waves that scatter multiple times inside the model. These include, for instance, interbed, intrasalt, and water-bottom multiples as well as conversions among them. We use an interferometry technique that is based on representation theorems for perturbed media and targets the reconstruction of specific primary reflections from multiply reflected waves. In this interferometry approach, we rely on shot-domain wavenumber separation to select the directions of waves arriving at a given receiver. Using a numerical walkaway (WAW) VSP experiment recorded by a subsalt borehole receiver array in the Sigsbee salt model, we use the interference of internal multiples to image the salt structure from below. In this numerical example, the interferometric image that uses internal multiples reconstructs the bottom- and top-of-salt reflectors above the receiver array as well as the subsalt sediment structure between the array and the salt. Because of the limited source summation in this interferometry example, the interferometric images show artifact reflectors within the salt body. We apply this method to a field walkaway VSP from the Gulf of Mexico. With the field data, we demonstrate that the choice of shot-domain wavenumbers in the target-oriented interferometry procedure controls the wavenumbers in the output pseudoshot gathers. Target-oriented interferometric imaging from the 20-receiver array recovers the top-of-salt reflector that is consistent with surface seismic images. We present our results with both correlation-based and deconvolution-based interferometry.
机译:地震干涉法已经成为用于成像钻孔地震数据的越来越多的兴趣的技术。我们证明内部倍数的干涉测量法可用于对井眼接收器阵列上方的目标成像。通过内部倍数,我们指的是在模型内部多次散射的所有类型的波。这些包括,例如,层间,盐内和水底倍数以及它们之间的转换。我们使用干涉技术,该技术基于扰动介质的表示定理,并针对来自多重反射波的特定主反射的重建。在这种干涉测量方法中,我们依靠散点域波数分离来选择到达给定接收器的波的方向。使用由Sigsbee盐模型中的盐下钻孔接收器阵列记录的数值走动(WAW)VSP实验,我们使用内部倍数的干扰从下面成像盐结构。在此数值示例中,使用内部倍数的干涉图像重建了接收器阵列上方的盐下和顶部反射器以及阵列和盐之间的盐下沉积物结构。由于该干涉测量示例中的源总和有限,因此干涉图像显示盐体内的伪影反射器。我们将此方法应用于墨西哥湾的现场可移动VSP。借助现场数据,我们证明了在面向目标的干涉测量过程中选择散布域波数可以控制输出伪散布道集中的波数。来自20个接收器阵列的面向目标的干涉成像可恢复与地面地震图像一致的盐顶反射器。我们介绍了基于相关和基于反卷积的干涉测量结果。

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