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Synthetic Seismograms and Wide-angle Seismic Attributes from the Gaussian Beam and Reflectivity Methods for Models with Interfaces and Velocity Gradients

机译:高斯光束和反射率方法的界面和速度梯度模型的合成地震图和广角地震属性

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摘要

The effects of interfaces and velocity gradients on wide-angle seismic attributes are investigated using synthetic seismograms. The seismic attributes considered include envelope amplitude, pulse instantaneous frequency, and arrival time of selected phases. For models with interfaces and homogeneous layers, head waves can propagate which have lower amplitudes, as well as frequency content, compared to the direct arrivals. For media with interfaces and velocity gradients, higher amplitude diving waves and interference waves can also occur. The Gaussian beam and reflectivity methods are used to compute synthetic seismograms for simple models with interfaces and gradients. From the results of these methods, seismic attributes are obtained and compared. It was found that both methods were able to simulate wide-angle seismic attributes for the simple models considered. The advantage of using the Gaussian beam method for seismic modeling and inversion is that it is fast and also asymptotically valid for laterally varying media.
机译:使用合成地震图研究了界面和速度梯度对广角地震属性的影响。考虑的地震属性包括包络振幅,脉冲瞬时频率和选定相位的到达时间。对于具有界面和均质层的模型,与直接到达相比,头波可以传播,其振幅和频率含量更低。对于具有界面和速度梯度的介质,更高振幅的潜水波和干扰波也会发生。高斯光束和反射率方法用于计算具有界面和梯度的简单模型的合成地震图。从这些方法的结果中,获得并比较了地震属性。结果发现,两种方法都能够为所考虑的简单模型模拟广角地震属性。使用高斯光束法进行地震建模和反演的优势在于,它对于横向变化的介质是快速且渐近有效的。

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