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, indicating major geological changes in the region.
• The findings suggest that the growth of the tibetan plateau is closely linked to the india-asia lithospheric collision.
• Geological insights were derived from analytical methods applied to the west kunlun range.
• Understanding this exhumation can provide critical insights into the geodynamic processes of plateau formation.

Abstract