The Joggins Fossil Cliffs, a renowned Carboniferous UNESCO World Heritage Site, is found along the shores of Chignecto Bay, Nova Scotia. This spectacular...
The Labrador-Baffin Seaway formed when Greenland pulled away from the North American Plate in the Early Cretaceous, with earliest seafloor spreading commencing...
North of the well-explored Jeanne d'Arc Basin and the emerging Flemish Pass area is a frontier region that is slowly gaining recognition as a petroleum...
The extensive passive margin of offshore eastern Newfoundland and Labrador developed during rifting and opening of the North Atlantic Ocean. Rift grabens are...
The Labrador Sea and Baffin Bay evolved through extension between North America and Greenland commencing in the Early Cretaceous, with seafloor spreading...
In a region where the West Orphan Basin (offshore Newfoundland) was once joined to its conjugate margin of Rockall Basin (offshore Ireland), we have mapped a...
The North American Stratigraphic Code ("the Code") addresses the naming of formal geologic units from a scientific per-spective. Guidelines based on scientific...
The Labrador margin developed through rifting as Greenland separated from the North American plate during formation of the Labrador Sea. Rifting began in the...
The passive margin offshore Labrador began forming during rifting in the Early Cretaceous, with seafloor spreading starting in the Maastrichtian and ending...
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