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Hottah Terrane comprises deformed metasedimentary and metavolcanic rocks cut by two distinct suites of plutons: a deformed suite of intermediate bodies (1.914-1.9 Ga) and a suite of undeformed leucogranites (1 .9-1.875 Ga). Sedimentary and volcanic rocks of the Bell Island Group, a basal unit of the Great Bear Magmatic Zone, unconformably overlie rocks of Hottah Terrane and are intruded by swarms of granitoid plutons and porphyries. One of the plutons, the Yen, has large areas of associated intrusion breccias of problematic origin. Both Hottah Terrane and Great Bear Magmatic Zone are cut by swarms of transcurrent faults. At least two of the faults had a component of vertical extension, as indicated by the existence of associated thrust faults similar to positive {lower structures found in other wrench zones. The recognition of a deformed arc-like plutonic suite generated between 1.914-1.9 Ga in the Hottah Terrane supports the interpretation that Coronation Margin developed in a back-arc setting.

Geology of the Rivière Grandin map area [hottah terrane and western Great Bear magmatic zone], District of Mackenzie