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Study on Method of Crosshole Seismic Tomography by Wavelet Transform

机译:小波变换的井间地震层析成像方法研究

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摘要

Combining the multiiesolution analysis (MRA) with tomography, this paper proposes a new method of crosshole seismic tomography named the wavelet multiscale seismic traveltime tomography. The method overcomes the drawbacks of linearized inversion depending on initial model and easily trapped by local minimum, and greatly improves the performance of linearized inversion. The results of numerical modeling and field application show that the main advantages of the new algorithm are: reaching the global minimum; inversion results less depending on the initial model; good stability; high resolution and high quality of tomography, and is suitable for non-uniform media with high contrast velocity, and also provides different resolution inverse results benefiting geological interpretation of tomographic images.
机译:将多溶质分析与断层扫描相结合,提出了一种井间地震层析成像的新方法,即小波多尺度地震走时层析成像。该方法克服了依赖初始模型进行线性化反演的缺点,容易被局部极小值所困,极大地提高了线性化反演的性能。数值建模和现场应用的结果表明,该新算法的主要优点是:达到全局最小值;实现全局最小值。反演结果较少,取决于初始模型;稳定性好;层析成像的高分辨率和高质量,并且适合于具有高对比度速度的非均匀介质,并且还提供了不同的分辨率反演结果,有利于层析成像图像的地质解释。

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