Vanadium behaviour in stratum-infiltration ore-forming process

It is shown that vanadium may be regular uranium satellite dike during stratum-infiltration ore formation if the process proceeds under alkali conditions (at pH over 8.2-8.3). Migrating vanadium deposition in stratum aqueous horizons may take place partially on acidic geochemical barrier in the form of uranyl-vanadates (on reduction of alkali waters pH) and, mainly, on reducing geochemical barrier in the form of different valence oxides - corvusite and vanoxite (V5+V4), doloresite and paramontroseite (V4), heggite (V4+V3), montroseit, as well as sulfide-patronite. Zones of stratum oxidation of rose-colored type are search criterium and index of exogenetic stratum-epigenetic vanadium ores