A quantitative model of development of magmatic and ore-magmatic systems under crests of mid-ocean ridges is constructed. Correct physical models of melting zone formation in approximation to active spreading, non-stationary dynamics of magma intrusion from a center of generation, filling of magma chambers of various shapes, feeding of fissure-type volcanoes, and retrograde boiling of melts during solidification of intrusive bodies beneath axial zones of spreading in crests of ridges are proposed. Physicochemical and mathematical theories of disintegration of multi-component solutions, growth of liquational drops of ore melts, and sublimation of components from magmatic gases are elaborated. Methods for constructing physically correct models of heat and mass transfer in heterophase media are devised. Modeling of development of magmatic and ore-magmatic systems on the basis of the Usov-Kuznetsov facies method and the Pospelov system approach are advanced. For quantitative models numerical circuits are developed and numerical experiments are carried out.

Supplement to: Sharapov, V N; Akimtsev, V A; Dorovskii, V N; Perepechko, Yu V; Cherepanov, A N (2000): Dinamika Razvitiya Rudno-Magmaticheskikh Sistem Zon Spredinga (Dynamics of Ore-Magmatic Systems in Spreading Zones). Publ. House of the Siberian Branch of RAS (Novosibirsk), 414 pp