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The internal zone of Wopmay orogen comprises a large klippe of 2.0-2.55 Ga gneissic rocks, termed Bent gneiss, and 1.90 Ga volcanic and sedimentary cover of the Grant-Akaitcho groups. Rocks of the Grant-Akaitcho groups probably formed near the leading edge of Hottah terrane just prior to the initiation of the Calderian orogeny. The gneissic basement and its cover were tectonically interleaved along west-vergent thrusts during the earliest stages of the Calderian orogeny. They were subsequently emplaced upon Slave craton. Lineations in the klippe and the autochthon indicate that the emplacement of the klippe was oblique dextral. Final Calderian compression resulted in the formation of large northerly-trending folds.

New Geological Developments in the Internal Zone of Wopmay Orogen, District of Mackenzie