Leveled model of scarn-magnetite deposits of the North and Middle Urals

The nature of deposit is exactly described by spatially-determined model. The concept of geological field is based on this model. The geological field of a deposit is the system comprising several coordinated structural levels. At every level finer mineral isolations (of higher orders) act as elements of heterogeneity. The carried out researches of scarn-magnetite deposits have allowed to create leveled model of deposits. In their internal structure there are eight natural levels.