The Churchill Craton is the northwest section of the Canadian Shield and stretches from southern Saskatchewan and Alberta to northern Nunavut. It has a very complex geological history punctuated by at least seven distinct regional tectonometamorphic intervals, including many discrete … See more • 2.69 Ga: deformation in the northern Hearne Domain. • 2.685 Ga: greenschist-grade metamorphism and deformation in the central Hearne Domain. • 2.60 Ga: granitoid plutonism across the northern Hearne and Rae … See more The Taltson Magmatic Zone (south of 60°N) is a composite continental magmatic arc and collisional orogen resulting from the convergence of the Buffalo Head terrane with the Archean Churchill craton. The Taltson basement (ca. 3.2–3.0 Ga and 2.4–2.14 Ga) and … See more • Rae Craton • Superior Craton See more A north-northwest-trending crustal segment transects from Kaminak Lake (central Hearne Domain) in the south to Yathkyed Lake (northern Hearne Domain) in the northwest, consisting of Archean supracrustal belts that preserve mostly Archean See more The Murmac Bay Group exposed in the southwestern half of the Western Churchill Craton, near Uranium City, Saskatchewan consists of a mixed … See more There is aggressive diamond exploration drilling in the south Slave Province, NWT, Churchill Craton (at the northwest corner of the Hudson Bay) and in Ontario. The Northwest Territories (NWT), … See more Webd’un orogène de collision résultant de la convergence du terrane de Buffalo Head et du craton archéen Churchill. Les gneiss de socle Taltson (ca. 3,2–3,0 Ga et 2,4–2,14 Ga) et les gneiss ...
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WebThe Canadian Shield spans much of northern Quebec, which is primarily underlain by the Superior Craton, a 160-mile thick section of stable continental crust formed beginning 4.03 billion years ago. In the northwest and at the northern tip of the Ungava Peninsula is the large Churchill Craton , which extends into Labrador and Nunavut as the ... WebThe Churchill craton is the northwest section of the Canadian Shield and stretches from southern Saskatchewan and Alberta to northern Nunavut. It has a very complex … WebLike all orogens (tectonic mountain belts), regardless of their time of formation, the THO formed as a result of the collision of tectonic plates, which in this case (Figure THO-2) were three Archean microcontinents: … crystal light up garland