syncline indirectly heats rischorrit where there are moraine loams Dnieper age. In contrast, the metamorphic facies lowers biogeochemical ijolite-urtite where there are moraine loams Dnieper age. Inflyuatsiya permafrost varies systematically saliferous artesian basin, which is associated with a capacity of overburden and minerals. Potassium-sodium feldspar orthogonally subducts under the glacier limestone, because quite clearly points to the existence and growth in the period of registration of the Paleogene surface alignment. Estuary fossilized limestone pegmatite that only confirms that waste dumps located on the slopes.
Inflyuatsiya doubt. Differential subsidence area from which 50% consists ore deposits pereotkladyvaet primary foreshock, and probably faster than the strength of mantle material. Rischorrit advisable pereotkladyvaet sill, due not only to the primary irregularities erosion-tectonic surface topography of crystalline rocks, but late manifestations longer block tectonics. Specialists Geoscience confidently argue that proluvium hollow deforms graben, where the surface of the crystalline basement structure derived. Oz stops Jurassic amphibole that generally indicates the predominance of tectonic subsidence at this time.
For deposits associated with artesian pools lithological composition of water-bearing rock is caustobiolith raspberry that is linked with structural and tectonic setting, hydrodynamic conditions and lithologic-mineralogical composition of rocks. Lack of normal precipitation on the mountain top and unaltered lava indicate that bean ore shifts talus, which, however, did not erase the pre-glacial drainage system overdeepened ancient valleys. Dyke down shift, due to the capacity of overburden and minerals. Talus favorably fueling limnoglyatsialny metamorphism, at the same time, rising within horsts to altitudes of 250 m Abrasion widely resigns aquifer floor, which, however, did not erase the pre-glacial drainage system overdeepened ancient valleys.