Hypogene and hypergene gold mineralization of Krilatovski-Chesnokovski оre field, the Middle Urals

The geological and geotectonic position of Krilatovski-Chesnokovski Оre Field, morphology, consistence and geology aspects of veined ore bodies of Krilatovski gold-quartziferous ore field are described. Chemical weathering crusts are divided into detrital girdle fabric and linophyric-karst. The gold placers of near in run offs of different age (K1, N11-2, N2, Q2-4) are well developed. Their dislocation is being controlled by Mesosoic erosion-geotectonic depression. The prospecting drilling has revealed in the bottom of depression the ore bearing crusts, that had experienced the overprint of argillization process. Depressions are reviewed as ore controlling morphologic structures onto ore grade mineralization not typical for this region.