In the northwest Himalaya deeply incised mountain ranges contrast with high-elevation, low-relief areas such as the Deosai plateau in northern Pakistan. Thermochronology data from the Deosai plateau, together with thermal history modelling, suggest that this plateau, along with other morphologically similar surfaces, is a remnant of an Eocene southwestern Tibetan plateau.
- Peter van der Beek
- Jérémie Van Melle
- Mohammad Latif