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首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Estimating surface-wave dispersion curves from 3D seismic acquisition schemes: Part 1 - 1D models
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Estimating surface-wave dispersion curves from 3D seismic acquisition schemes: Part 1 - 1D models

机译:通过3D地震采集方案估算表面波频散曲线:第1部分-1D模型

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摘要

Surface-wave analysis is based on the estimation of surface-wave dispersion curves, which are then inverted to provide ID S-wave velocity profiles. Surface-wave dispersion curves can be extracted from P-wave records obtained in seismic exploration and used to characterize the ground structure at a shallow depth. Dispersion curve estimation using 2D wavefield transforms is well-established for 2D acquisition schemes (in-line source and receiver spread). It is possible to extract surface-wave dispersion curves using 2D wavefield transforms from 3D seismic data acquired with any acquisition scheme. In particular, we focus on areal geometry and orthogonal geometry, and we provide a method based on the analysis in the offset domain and the f-k multiple signal classification (MUSIC) transform. We assess the performance of the method on synthetic and field data concerning 1D sites.
机译:面波分析基于面波频散曲线的估计,然后将其反转以提供ID S波速度曲线。可以从地震勘探中获得的P波记录中提取表面波频散曲线,并将其用于表征浅深度的地面结构。对于2D采集方案(在线源和接收器扩展),使用2D波场变换的色散曲线估计是公认的。可以使用2D波场变换从任何采集方案采集的3D地震数据中提取表面波频散曲线。特别是,我们专注于平面几何和正交几何,并提供了一种基于偏移域分析和f-k多信号分类(MUSIC)变换的方法。我们评估该方法在涉及一维站点的合成数据和现场数据上的性能。

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