利用发射-接收时间变换提取表面波

Y. Ding, A. Malehmir
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引用次数: 0

摘要

地震数据包含由不同类型的波携带的丰富信息,如直达波(P波和s波)、反射波、衍射波和表面波。为了利用特定类型的波,需要将这个想要的信号与其他信号隔离开来。针对沿二维剖面采集的地震数据,我们提出了一种主要根据其在发射-接收-时间域的几何性质提取和/或去除色散表面波的方法。我们首先将所有镜头集合到一个带有镜头位置、接收器位置和时间尺寸的伪3D数据中。投篮-接球时间域使我们能够沿着不同的维度处理数据,而不仅仅局限于投篮域。在一维速度模型的假设下,我们发现在射孔集合中的色散面波在时间等时线上表现为线性,该等时线切断了所有射孔和接收器。面波在时间等时线上的线性几何特性使我们能够高效地提取它们,例如使用基于曲线的变换。通过对存在面波的时间样本沿时间等时线应用该方法,可以从伪三维数据中提取出面波。我们用一个合成数据和一个现场数据来举例说明这种方法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Surface-Waves Extraction Using a Shot-Receiver-Time Transformation
Summary Seismic data contain rich information carried by different types of waves, such as direct arrivals (P- and S-waves), reflections, diffractions and surface-waves. In order to utilize a specific type of wave, one needs to isolate this wanted signal from others. We propose a method to extract and/or remove mainly the dispersive surface-waves based on their geometrical property in the shot-receiver-time domain for seismic data acquired along 2D acquisition profiles. We first assemble all shot gathers into a pseudo 3D data with dimensions of shot locations, receiver locations, and time. The shot-receiver-time domain enables us to process the data along different dimensions, not restricted to the shot domain only. With the assumption of a 1D velocity model, we find that the dispersive surface-waves in a shot gather behave linearly in a time isochrone, which cuts through all shots and receivers. The linear geometrical property of the surface-waves in the time isochrone allows us to extract them efficiently and effectively using for example curvelet-based transforms. By applying the method along the time isochrones for the time samples where surface-waves are present, surface-waves can be extracted from the pseudo 3D data. We exemplify this method using a synthetic data and a field data.
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