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A New Scheme for the Solution of Inverse Problems in Seismic Tomography

机译:解决地震层析成像反问题的新方案

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Long-term experience in construction of seismic tomographic images in different regions of the world indicates the existence of the problem of ambiguity in results. For example, velocity sections obtained on the basis of numerical solutions of the systems of linear equations are not always comparable with the data of petrology and geology. The main cause is in the unknown level of the real error in each seismic observation, which leads to a distortion in the real image. A computational scheme in the linear formulation is suggested for the first time in the practice of the solution to tomographic problems, which allows us to avoid a significant influence of errors in the observations on the inverse result. The stability of the solution is guaranteed by a new regulation method in seismic tomography. The efficiency of the developed approach is proved by its ability to restore a complex model of the fracture zone within an admissible small error. Such a very high quality was not gained by the modern methods based on the standard approach.
机译:在世界不同地区构造地震层析图像的长期经验表明,结果存在歧义性问题。例如,基于线性方程组的数值解获得的速度剖面并不总是与岩石学和地质学数据可比。主要原因是每次地震观测中真实误差的未知水平,这导致真实图像失真。在解决层析成像问题的实践中,首次提出了线性公式中的计算方案,这使我们避免了观测误差对反演结果的重大影响。解决方案的稳定性通过地震层析成像中的新调节方法得以保证。所开发方法的效率通过其在允许的小误差范围内恢复复杂的断裂带模型的能力证明。基于标准方法的现代方法无法获得如此高的质量。

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