地震层析成像的多尺度方法

Bin Wang, L. Braile
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引用次数: 1

摘要

地震层析成像的目的是推导出速度模型。本文描述了一种多尺度迭代求解速度模型的方法。在迭代过程的早期,我们应用大尺度平滑约束来推导速度模型的大尺度特征。随着数据不拟合的减少,我们逐渐减少平滑约束,为导出的模型添加更精细的细节。我们的方法的关键组成部分是有效地控制一个衍生模型的平滑性。为了实现这一点,我们开发了一种基于随机反演的平滑约束的新实现。对于离散和均匀网格模型,可以证明我们基于随机反演的新实现与基于正则化方法的传统实现是等效的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A multi-scale approach for seismic tomography
The goal of seismic tomography is to derive a velocity model. In this paper, we describe a multi-scale approach which iteratively derives a velocity model. In the early stage of the iterative process, we apply large smoothing constraints to derive the large scale features of the velocity model. As the data misfit reduces, we gradually reduce the smoothing constraints, adding finer details to the derived model. The key component of our approach is effective control of the smoothness of a derived model. To achieve this, we have developed a new implementation of smoothing constraints based on stochastic inversion. For a discrete and uniformly gridded model, it can be shown that our new implementation based on the stochastic inversion is equivalent to the conventional implementation based on the regularization method.
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