This paper presents a comparison of the spectrum of different geochemical dispersion patterns of Zolotoe deposit with actual data obtained from detailed mineralogical studies, in order to identify mineral composition of ore by variability of the geochemical spectrum of ore-forming elements. Despite the fairly resistant ore associations, traceable at all stages of the evolution of geochemical patterns (gold-arsenopyrite-pyrite), the processes of oxidation and weathering of ore deposits greatly affect the possibilities of indicator satellite elements of gold.