Deep-seated processes in the Alpine geosyncline of the Ukrainian Carpathians
© Gordienko V.V., Usenko O.V.
Deep-seated processes in the Alpine geosycline of the Carpathians are considered. Their model is constructed according to an advection - polymorphic hypothesis. The speeds of deposits accumulation have been calculated. The depths of magma sources in the crust and upper mantle for different stages of geosyncline development are determined. The conformity of the process parameters, calculated and known on the geological-geophysical data, is shown.