Spatially variable syn- and post-Alleghanian exhumation of the Central Appalachian Mountains from zircon (U-Th)/He thermochronology

To assess spatial and temporal patterns of Phanerozoic orogenic burial and subsequent exhumation in the central Appalachian Mountains, we present mid-temperature zircon (U-Th)/He (ZHe; closure temperature [TC] = 140-200°C) dates for 10 samples along a 225 km, strike-perpendicular transect spanning t...

Ausführliche Beschreibung