Cosmostructural model of the Kalgutinskiy rare-metal deposit area (Mountainous Altai)
The cosmostructures of the Kalgutinskiy rare-metal deposit area (Mountainous Altai) have been studied on the materials of multispectral space shooting Landsat ETM+ and radar-tracking shooting SRTM. The area is localized inside of the large ring structure of the complex construction, characterized by the long multistage (multipulse) development. Immersing of the structure root (focus) part from the north-northwest to the east - southeast is established. The position of the ring structure is supervised by crossing node of fracture zones of northwest, northeast and northeast - sublatitudinal directions. The Kalgutinskiy granite massif and the deposit itself are located in the internal belt of structure in the ring with 15,2 km in diameter. The perspective of ore-bearing ability of the southeast part of the area is highly evaluated in connection with development of small ring structures of the second type.