Exhumation history and tectonic inheritance of the Frontenac Arch (SE Ontario, Canada) from low-temperature thermochronology
The Frontenac Arch is a low-relief, NW-SE–oriented exposure of Grenvillian basement that connects the southeastern Canadian Shield with the Adirondack Mountains in the United States. The absence of low-temperature thermochronological constraints has limited our understanding of how this feature participated in, or resp...