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Shear Wave Velocity Inversion from the Seismic Surface Waves Using Data Adaptive Wavelets

机译:利用数据自适应小波从地震地表波反演剪切波速度

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We study the dynamic and physical properties (shear velocity, seismic attenuation, stiffness and density) of marine sediments from seismic-acoustic records of surface/interface waves along the water-seabed boundary. Accurate models of the marine sediments properties in the shallow subsurface are critical in many disciplines. For example, in oil and gas exploration knowledge of the sedimentary acoustic properties helps to improve the shear wave static corrections, it provides shear strength modulus in the geotechnical engineering, helps to estimate acoustic loss for sonar operation in the shallow water. Our method relies on using dispersive characteristics of the seismic surface waves which can be further inverted for the shear velocities as function of depth and distance. We use wavelet analysis to separate surface wave modes and extract their group and phase velocities. To improve the accuracy in imaging of the surface wave modes we have developed and applied a new tool - adaptive wavelet which parameters are defined directly from the data. We demonstrate how these wavelets can be employed to provide more accurate shear waves velocities estimates.
机译:我们从沿水-海底边界的表面/界面波的地震声记录中研究海洋沉积物的动力学和物理特性(剪切速度,地震衰减,刚度和密度)。在许多学科中,浅层地下海洋沉积物特性的准确模型至关重要。例如,在油气勘探中,对沉积声特性的了解有助于改善剪切波的静态校正,在岩土工程中提供剪切强度模量,有助于估算浅水声纳操作的声损耗。我们的方法依赖于利用地震面波的色散特性,该特性可以进一步将剪切速度作为深度和距离的函数进行反演。我们使用小波分析来分离表面波模式,并提取它们的群速度和相速度。为了提高表面波模式成像的准确性,我们开发并应用了一种新工具-自适应小波,该参数直接从数据中定义。我们演示了如何使用这些小波来提供更准确的剪切波速度估计。

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