Supplemental Material: Late Miocene rapid exhumation in the West Kunlun range: Insights into Tibetan Plateau growth and India-Asia lithospheric collision

Key Points

• Rapid exhumation occurred in the late miocene period, accelerating the growth of the Tibetan Plateau.
• Insights from the West Kunlun Range indicate significant geological activity associated with the India-Asia collision.
• The findings suggest that tectonic forces contribute to the ongoing evolution of the Tibetan region.
• Geological evidence presented provides a clearer understanding of the lithospheric processes over millions of years.

Abstract