近地表二维Vs模型表面波频散曲线反演新处理流程

X. Song, G. Liu
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引用次数: 0

摘要

本文建立了一种利用瑞利面波频散曲线估计近地表二维Vs速度模型的处理流程。采用频率分解法提取瑞利面波色散能量图。但由于提取的色散能量图分辨率较低,引入窗口叠加法,将同一窗口内多个射击点的色散能量叠加在公共窗口中心的色散能量图上。然后沿采集线方向移动窗口,提取不同位置的色散能量图。在相速度周期网格上进行二维搜索,从叠加的能量峰中选择色散点。加窗和叠加也可以平滑模型的横向变化,提高信噪比。然后,采用基于奇异值分解的阻尼最小二乘法对一维Vs速度进行反演,并对反演的一维Vs速度进行插值得到二维Vs速度剖面;Sylvain pasquet和Ludovic bodet(2017)分享的黄石国家公园模拟数据和实际数据显示了处理过程的有效性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
New processing flow for surface wave dispersion curve inversion of near surface 2-D Vs model
Summary In this paper, a processing flow for estimating the near surface 2-D Vs velocity model using Rayleigh surface wave dispersion curve is established. Rayleigh surface wave dispersion energy diagram is extracted by frequency decomposition method. However, due to the low resolution of the extracted dispersive energy map, the window superposition method is introduced to superimpose the dispersive energy of multiple shot points in the same window on the dispersive energy map in the center of the common window. Then move the window along the direction of the acquisition line to extract the dispersive energy map at different positions. 2-D search is carried out on the periodic grid of phase velocity, and the dispersion points are selected from the superimposed energy peaks. Windowing and stacking can also smooth the lateral changes of the model and improve the signal-to-noise ratio. Then, the singular value decomposition based damped least square method is used to inverse the one-dimensional Vs velocity, and the inverse 1-D Vs velocity is interpolated to obtain the 2-D Vs velocity profile. The simulation data and the actual data of Yellowstone National Park shared by Sylvain pasquet and Ludovic bodet (2017) show the effectiveness of the processing process.
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