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The basement of the western European and eastern Canadian shelves is underlain in the northwest by metamorphosed terrains predating the late Precambrian; in the southeast, Cadomian deformations are widespread. These eratonic regions were broken up by the opening of two oceans during Paleozoic time. Remnants of Paleozoic ocean crust are now preserved in the sutures of the Iapetus and Theic oceans. Later deformations, related to the collision between Laurussia and Gondwanaland, resulted in the development of three shear belts, oriented east to west, between middle and late Carboniferous time. Just before the Mesozoic opening of the North Atlantic, a large dextral shear belt developed between Labrador and the Bay of Biscay, crosscutting all the previously developed structures.

The Main Basement Features Recognized in the Northern Part of the North Atlantic Area