Regime of morphostructures development, their inheritance, the links between primary sources and zones of accumulation of placer's material, the presence of chemical weathering crusts appear the most important factors, which define morphogenetic types and the extent of placer deposits. These factors of placers formation were strongly manifested at the certain periods of the history of relief.
Regime of morphostructures development, their inheritance, the links between primary sources and zones of accumulation of placer's material, the presence of chemical weathering crusts appear the most important factors, which define morphogenetic types and the extent of placer deposits. These factors of placers formation were strongly manifested at the certain periods of the history of relief.
The authors declare that there are no conflicts of interest present.