Mantle Transition Zone

Mantle Transition Zone Structure in SE Tibet

Using Receiver Function method to estimate the topography of MTZ under SE Tibet

Lateral variation of the mantle transition zone beneath the Tibetan Plateau: Insight into thermal processes during Indian–Asian collision

The Indian plate began to subduct under the Eurasian plate in the late Mesozoic. Since the Eocene, continuous continental collision has resulted in the uplift of the Tibetan Plateau with extensive volcanic activity. Geophysical and geochemical …