Deep seated processes within the Cimmerian geosyncline of the Scythian plate
© Gordienko V.V., Usenko O.B.
The deep-seated processes within the Cimmerian geosyncline of the Scythian Plate are considered. Their model is constructed according to the advection-polymorphic hypothesis. The speeds of deposits accumulation are designed. The depths of the centers of magmas in the crust and upper mantle for different stages of geosyncline development are determined. The conformity of the process parameters, calculated and known according to the geological data, is shown.