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The Glennie domain of the Trans-Hudson Orogen (THO) is characterized by Paleoproterozoic island arc volcanogenic assemblages and granitoid rocks thrust as sheets over the Archean Saskatchewan craton prior to terminal collision between the Archean Rae-Hearne and Superior cratons. Four discrete deformation events have been recorded in the domain. The D1 and D2 events are associated with the southwestward-directed...