Relationship between mercury and arsenic mineralization in the Sarasa ore zone (Gornyy Altay)

Granite gneiss, gneiss, and granite domes of Central Karelia are developed near the junction zone between two tectonic structures, the Western anticlinorium of the Belomorides and the East Karelian zone of the Karelides, The established regular restriction of both shows and deposits of a number of mineral resources to the surroundings of the domes is of importance in forecasting and the future direction of exploration work in this region. —Authors.