Mineral cooling ages reveal three pulses when uplift and erosion exposed deeper rocks, showing that Southeast Tibet grew outward, step by step, over roughly 80 million years.
Djordje Grujic
Editor, Tectonics
Editor, Tectonics
Mineral cooling ages reveal three pulses when uplift and erosion exposed deeper rocks, showing that Southeast Tibet grew outward, step by step, over roughly 80 million years.