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从理论上讲,磁异常对数功率谱可用来直接估算场源埋深,可理论的推断是以理想条件为前提的,实际应用中难以完全满足这些条件,从而可能导致埋深估算误差.国内外已有些作者对用此法的影响因素做过一些研究,给出了一些很有用的结论,但这些研究都仅限于其中几个方面,不甚全面,也没有给出不利条件下的处理方法.至于磁性地质构造磁异常对数功率谱埋深估算问题,迄今还没有看见有详细的报导.我们在对磁异常对数功率谱埋深估算方法作简单讨论之后,把其应用于二度和三度地质体以及地质构造模型磁异常解释,在此基
Theoretically, the magnetic anomaly logarithmic power spectrum can be used to directly estimate the depth of the field source. The theoretical inference can be premised on the ideal conditions, which can not be fully satisfied in practical applications, which may lead to the estimation of the depth of the buried. Some authors have already done some research on the influencing factors of this method and have given some useful conclusions. However, these studies are limited to a few aspects, are not comprehensive, and do not give any treatment under unfavorable conditions As for the magnetic geological structure of magnetic anomalies logarithmic power spectral depth estimation problem, so far there is no see to have a detailed report.We magnetic anomaly logarithmic power spectral depth estimation method for a brief discussion, it is applied to the second degree and Third-degree geologic bodies and geomagnetic structural anomalies are explained here