Local Rapid Exhumation and Fast Cooling in a Long-lived Paleoproterozoic Orogeny

Abstract The exhumation and cooling rates of high-grade metamorphic rocks are crucial for inferring orogenic processes and understanding the regimes of heat transport in the Earth’s crust. Quantification of these rates remains challenging for Precambrian terranes, because the temporal resolution of geochronology becomes coarser in deeper geological time. This limitation is partly reflected by a striking lack of Proterozoic or older short-duration events (