Remnants of PaleoProterozoic Volcanic Arc Bonnetia Found in Yukon

The Wernecke igneous clasts in Yukon, Canada: fragments of the Paleoproterozoic volcanic arc terrane Bonnetia

Authors:

Alexander B. Nielsen, Derek J. Thorkelson, H. Daniel Gibson and Daniel D. Marshall

Abstract:

The Wernecke igneous clasts consist of blocks of plutonic and volcanic rock that range up to hundreds of metres in size. These clasts occur exclusively within zones of hydrothermal breccia (Wernecke Breccia) which are widespread in central and northern Yukon. The breccia zones are hosted by the Wernecke Supergroup and have been dated by U-Pb titanite at 1599 Ma. Four U-Pb zircon ages on the Wernecke igneous clasts (1714-1706 Ma) demonstrate that the clasts are older than the Wernecke Supergroup (less than 1.64 Ga) and indicate that the clasts were not derived from dykes within the Wernecke Supergroup. Instead, the clasts were derived from an obducted terrane named Bonnetia. Geochemical characteristics of the Wernecke igneous clasts infer that Bonnetia formed as a volcanic arc with a component of within-plate magmatism. Neodymium mantle depletion ages of 2080-2760 Ma suggest that the arc was built on older continental crust. Consequently, Bonnetia may have been a volcanic arc, possibly built on a rifted fragment of Laurentia, on another continental fragment, or possibly on the leading edge of another continent. The subsequent event of breccia-formation may represent a hydrothermal response to obduction-caused tectonic loading of the crust. The characterization of Bonnetia as a volcanic arc complex that underwent obduction requires that northwestern Laurentia was flanked by an ocean basin in the late Paleoproterozoic