Slip tectonics of the Khingan-Olonoysky tin ore district, and structural control over the ore bodies

The paper presents the facts showing that the location of ore deposits and occurrences in the Khingan-Olonoysky tin ore district is determined by conjugated systems of deep and shallow strike-slip faults, developed above the fluid-and metal plume. It is considered the criteria for en echelon shear systems distribution and the ore bodies controlled by them, as for the pulling apart structures. The ore-controlling en echelon shear systems predict the direction and the areas, most favorable for blind mineralization.