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.
The main team of the research is study of the nature shaping geochemical anomaly of gold. That will allow answering the question about reason of high level anomaly of gold. The analysis of the forms of finding gold and study of its behavior have shown that process of the destruction ore mineral occurs stand gold from bedrock and accumulation it in secondary aura in the most soluble phase (the phase of sulfide and metal) that prevents their further redistribution.
