与电阻率测深相似,激发极化测深(以下简称ВП_(вэз))也能用来确定矿体的埋藏深度。由于岩石矿物激发极化特性比较稳定,在金属矿床上用激发极化测深来确定矿体埋藏深度,比电阻率测深要优越得多。但由于目前还没有一套系统量板,而且除了几种比较简单的情况以外,理论公式的推导问题也还未全部解决。因此,在各种地质地形情况下, Similar to resistivity sounding, induced polarization sounding (hereinafter referred to as ВП_ (вэз)) can also be used to determine the burial depth of the ore body. Because of the relatively stable excitation-induced polarization characteristics of rock minerals, the determination of the burial depth of ore bodies by using stimulated polarization soundings on metallogenic deposits is far superior to resistivity sounding. However, due to the fact that there is not a set of system board yet, and in addition to a few simpler cases, the derivation of the theoretical formula has not yet been fully solved. Therefore, in a variety of geological topography,