地震记录的一维反演

E. Eisner
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引用次数: 4

摘要

地震勘探试图从可达地表的观测中恢复地球的声学结构。沉积历史常常使平面层状模型成为构造的合理的第一近似。现场技术不对应于平面波的使用,但将讨论从数据中提取这种观测等效的方法。因此,考虑这种一维情况下的反演问题是很有意义的。本文将提出一种进行这种反演的方法,并讨论相应的问题。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
One-dimensional inversion of seismograms
Seismic exploration attempts to recover the acoustic structure of the earth from observations made at the accessible surface. Depositional history often makes a plane-layered model a reasonable first approximation to the structure. Field techniques do not correspond to the use of plane waves, but a method of extracting the equivalent of such observation from data will be discussed. Thus it is of interest to consider the inversion problem for this one-dimensional case. One method for performing such an inversion will be presented, and attendant problems will be discussed.
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