Circum-Superior Belt | |
|---|---|
 Map of cratons, orogenies and the Circum-Superior Belt. Areas associated with the Circum-Superior Belt include: A = New Quebec Orogen, B = Cape Smith Belt, C = Eastern Hudson Bay, D = Thompson region, E = Animikie Basin, F = Western interior of Superior craton. | |
| Location | Manitoba, Ontario, Nunavut, Quebec |
| Part of | Canadian Shield |
| Age | Paleoproterozoic |
The Circum-Superior Belt is a widespread Paleoproterozoic large igneous province in the Canadian Shield of Northern, Western and Eastern Canada.[1][2][3][4] It extends more than 3,400 km (2,100 mi) from northeastern Manitoba through northwestern Ontario, southern Nunavut to northern Quebec and into western Labrador. Igneous rocks of the Circum-Superior Belt are mafic-ultramafic in composition, deposited in the Labrador Trough near Ungava Bay, the Cape Smith Belt near the southern shore of Hudson Strait and along the eastern shore of Hudson Bay in its northern portion; the Thompson and Fox River belts in the northwest and the Marquette Range Supergroup in its southern portion. The Circum Superior Belt also hosts a rare example of Proterozoic Komatiite, in the Winnipegosis komatiite belt.[3][5]
A number of magmatic features are present in the Circum-Superior Belt, including dikes, sills and volcanics that comprise geologic formations. This geologic belt is considered to be a large igneous province because its magmatic rocks were emplaced over an extremely short geological time span.[3][4] Even though the Circum-Superior Belt was emplaced during an extremely short geological time span, the associated magmas were probably derived from a number of separate sources.[6]
Most of the Circum-Superior Belt lies along the margin of the Superior Craton, which is the most extensive fragment of Archean crust on Earth.[6] The Circum-Superior Belt contains two large copper-nickel mining districts; the nickel-bearing Thompson Belt at the northwestern portion of the Superior craton and the Cape Smith Belt at the northern portion of the Circum-Superior Belt.
- ^ Baragar, Scoates. "The Circum-Superior Belt: A Proterozoic plate margin?". Developments in Precambrian Geology. 4: 297–330. doi:10.1016/S0166-2635(08)70017-3.
- ^ Minifie, Kerr, Ernst, Hastie, Ciborowski, Desharnais, Millar (2013). "The northern and southern sections of the western ca. 1880 Ma Circum-Superior Large Igneous Province, North America: The Pickle Crow dyke connection?". Lithos. 174: 217–235. Bibcode:2013Litho.174..217M. doi:10.1016/j.lithos.2012.03.017.
{{cite journal}}: CS1 maint: multiple names: authors list (link) - ^ a b c Waterton, Pearson, Kjarsgaard, Hulbert, Locock, Parman, Davis (2017). "Age, Origin, and Thermal Evolution of the ultra-fresh ~1.9 Ga Winnipegosis Komatiites, Manitoba, Canada". Lithos. 268–271: 114–130. Bibcode:2017Litho.268..114W. doi:10.1016/j.lithos.2016.10.033.
{{cite journal}}: CS1 maint: multiple names: authors list (link) - ^ a b Ciborowski, Minifie, Kerr, Ernst, Baragar, Millar (2017). "A mantle plume origin for the Palaeoproterozoic Circum-Superior Large Igneous Province". Precambrian Research. 294: 189–213. Bibcode:2017PreR..294..189C. doi:10.1016/j.precamres.2017.03.001.
{{cite journal}}: CS1 maint: multiple names: authors list (link) - ^ Waterton, Pearson, Mertzman, Mertzman, Kjarsgaard (2020). "A fractional crystallisation link between komatiites, basalts, and dunites of the Palaeoproterozoic Winnipegosis Komatiite Belt, Manitoba, Canada". Journal of Petrology. 61 (5). doi:10.1093/petrology/egaa052.
{{cite journal}}: CS1 maint: multiple names: authors list (link) - ^ a b "Ca. 1880 Ma Circum-Superior LIP". Ernst, Richard E. Retrieved 2010-01-10.[permanent dead link]