Dewey & Casey (2013) present a model for generation of the Bay of Islands Complex and its metamorphic sole that is anchored on intra-oceanic subduction initiation at a ridge–transform boundary. Several aspects of this model are inconsistent with a wealth of geological relationships and cannot readily accommodate the geological complexity of associated units in Newfoundland. Their model presents an alternative to the models of Waldron & van Staal (2001) and van Staal et al. (2007, 2013), which propose formation of the Baie Verte oceanic tract, including the Bay of Island Complex, after a Late Cambrian collision between...

You do not currently have access to this article.