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Wopmay orogen information


Geological map of north-western Canada. Wopmay orogen marked with D.

The Wopmay orogen is a Paleoproterozoic orogenic belt in northern Canada which formed during the collision between the Hottah terrane (north of the Hottah Lake), a continental magmatic arc, and the Archean Slave Craton at about 1.88 Ga (billion years). The collision lead to the short-lived Calderian orogeny.[1] The formation was named for Wilfrid Reid "Wop" May, OBE, DFC (April 20, 1896 – June 21, 1952), a Canadian flying ace in the First World War and a leading post-war aviator.

It is approximately 500 km along the north–south axis, and 200 km along the east–west axis at its widest point, tapering at both the northern and southern ends.[2][failed verification]

  1. ^ Hildebrand, Hoffman & Bowring 2010, Abstract
  2. ^ "Comparisons of the 2005 Geologic Map of North America with the 1965 Map, Areas 1-4; Area 2, Northwestern Canadian Shield". Geology and Environmental Change Science Center. United States Geological Survey (USGS). Retrieved 22 May 2016.

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Wopmay orogen

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St-Onge, M R; King, J E; Lalonde, A E (1988). "Geology, East - Central Wopmay Orogen, District of Mackenzie, Northwest Territories". doi:10.4095/130452....

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