кільцеві структури

Most of the ore deposits are located in the ore-magmatic systems, which are spatially and genetically connected with the ring structures. Studying of the geology and all available map materials allows to detect the type and background of different signs of deposit mineralization and to develop the criteria for exploration of mineral deposits.

Based on the results of three-dimensional gravity modeling, listric faults have been mapped on the Ukrainian Shield for the first time. The relationship of the faults with ring structures has been established.