This article considers qualitative and quantitative interpretation of spectral decomposition results on the basis of a deposit in Western Siberia. Spectral decomposition as a method of time-frequency analysis is getting extensively used in geophysical during recent years. This fact makes relevant to consider geological structure prediction algorithms on spectral amplitude characteristics. The study proposes a new approach to the interpretation of spectral data - frequency pseudo-cube, which on the one hand allows to optimize interpretation process, on the other hand, allows to use new analysis technics such as principal component analysis and cluster analysis. Approaches to interpretation discussed on a single case that allows to perform a comparative analysis of the methods and to determine the most informative one within particular subject of study.