Low‐temperature thermochronometry along the Kunlun and Haiyuan Faults, NE Tibetan Plateau: Evidence for kinematic change during late‐stage orogenesis

Abstract The Tibetan Plateau is a prime example of a collisional orogen with widespread strike‐slip faults whose age and tectonic significance remain controversial. We present new low‐temperature thermochronometry to date periods of exhumation associated with Kunlun and Haiyuan faulting, two major s... View More