East European Platform or Russian Platform is a large and flat area of the East European Craton covered by sediments in Eastern Europe spanning from the Ural Mountains to the Tornquist Zone and from the Peri-Caspian Basin to the Barents Sea.
Over geological time the platform area has experienced extension, inversion and compression.
The Mesoproterozoic Jotnian sediments of the Baltic area are examples of a "quasiplatform".
[4] The oldest preserved continuous sedimentary cover in the platform date to the Vendian about 650 million years ago.
[1] The platform hosts numerous ancient rifts or aulacogens some of which date to the Riphean of the Proterozoic.