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The East Coast of Canada is normally divided in to three areas: the Nova Scotian margin when you look at the south, the Newfoundland margin at the heart and eastern, plus the Labrador margin into the north (Figure 1). These margins formed in the past 200 million years whilst the supercontinent of Pangea rifted apart, first as North America separated from Africa after which since it separated from European countries and Greenland (Figure 2). These episodes of rifting thinned and heated the crust that is continental lithosphere, which in turn subsided to make a complex pair of marginal basins. Huge amounts of sediment have actually since accumulated during these basins and created sources and traps for hydrocarbon deposits. Exploration activity to get and exploit these resources, mainly from seismic pages and boreholes associated with previous three decades, has triggered the current manufacturing of oil off Newfoundland and gasoline off Nova Scotia. Exploration tasks of both commercial and systematic activities have additionally yielded a wealth of fundamental information which has had significantly enhanced our knowledge of the essential procedures of lithospheric expansion and continental rifting that have actually formed these margins and their hydrocarbon resources.

Figure 1. Map of Eastern Canada with places of Nova Scotian, Newfoundland and Labrador continental margin sections. Dashed lines give locations of Appalachian front side (AF) and Grenville Front (GF), which divide the continental areas into three major provinces that are geological. Continue reading “Tectonic development of this East Coast of Canada”