In 1958, I.V.Litvinenko laid the foundation for seismic studies of the consolidated earth crust on the Baltic Shield: for the first time, depth seismic soundings were performed in Karelia.
Глубинные сейсмические исследования (Г C 3) в восточной части Балтийского щита выполнены совместными усилиями нескольких организаций (ПГО "Севзапгеология", ЛГИ и др.) под научным руководством профессора И.В.Литвиненко ...
In 1980 in the northwestern part of Ladoga and southwestern Karelia the production and geological association Sevzapgeologia and the Problem Research Laboratory of geological and geophysical studies of the Baltic Shield of the G.V.Plekhanov Leningrad Mining Institute conducted deep seismic studies by methods of deep seismic sounding and exchange waves from distant earthquakes (MOB3) along the profile and the Problem Research Laboratory of Geological and Geophysical Research of the Baltic Shield of the Leningrad Year Institute named after G.V. Plekhanov conducted depth seismic studies by methods of depth seismic sounding (DSS) and exchange waves from distant earthquakes (MOVZ) along the profile of Lahdenpokhya - Lake Segozero, which is hereinafter referred to as the Priladozhsky ...
In 1976-1979, the production and geological association Sevzapgeologia and the Problem Research Laboratory of Geological and Geophysical Research of the Baltic Shield of the Leningrad Mining Institute performed depth seismic surveys (DSR) in Central Karelia along the profile of the city of Kem - Lake Tulos, which is a continuation of the international geotraverse I, passing from the Alps to the Baltic Shield through the territories of the FRG, Czechoslovakia, Poland and the USSR ...
На Балтийском щите, в зарубежной и советской его частях, к настоящему времени проведен большой объем работ методами взрывной и обычной сейсмологии, позволяющий определить подошву консолидированной коры — поверхность Мохоровичича (М) — в различных его районах ...
