ГЛУБИННОЕ СТРОЕНИЕ РУДНЫХ РАЙОНОВ ФЕННОСКАНДИНАВСКОГО И УКРАИНСКОГО ЩИТОВ

New interpretation of geological and seismic data has revealed a correlation of surface structures of large endogenous ore districts of the Fennoscandian and Ukrainian shields with Moho topography and local crustal inhomogeneities. As a result, models of the deep structure of Pechenga, Onega and Kirovograd ore districts based on consistent analysis of geological and seismic data were constructed and compared.