Siberian Federal University 
- Issue
- Journal of Siberian Federal University. Engineering & Technologies. 2008 1 (1)
- Authors
- Tsykin, Rostislav A.
- Contact information
- Ростислав А. Цыкин: Сибирский федеральный университет,660041 Россия, Красноярск, пр. Свободный, 79, e-mail:
- Keywords
- hypergene; manganese ores; residial; infiltration; hydrogenous mineralization; deposits; show of ores
- Abstract
The concentrations of oxide and hydroxide manganese and iron-manganese ores of variable quality are prospected in the area. The residual ores are specified, the dimention and quality of such deposits are mainly determined by primary carbonate mineralization. The residual-infiltration ores appeared as a result of evacuation and transition of manganese and assotiate elements, in case of existence of primary ores or manganese-bearing rocks. The hydrogenous mineralization (in the narrow sense) settle by underground water and sometime in the zones of interbedded water discharge (Sejbinsk-1 deposit). The infiltration genetic species of smaller scale are formed in deposition and replacement places of jointing rocks by ores minerals. In most cases the hypergene mineralization has been ranked as show of ores with the residual ores to form the resourses of oxidation zones of the Mazulsk, Usinsk and Nicolaevsk deposits. The residual-infiltration ores are presented by the middle-sized Porozhinsk deposit.
- Pages
- 3-16
- Paper at repository of SibFU
- https://elib.sfu-kras.ru/handle/2311/732
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