DEEP STRUCTURE OF ORE DISTRICTS OF THE FENNOSCANDIAN AND UKRAINIAN SHIELDS

Abstract

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.

Keywords

• метод глубинного сейсмического зондирования (гсз)
• метод обменных волн землетрясений (мовз)
• поверхность мохо
• кора
• мантия