Study reveals strong uplift of northeastern Tibet Plateau in late Miocene
Northeastern Tibet Plateau uplift and impact on precipitation. Credit: Miao Yunfa
The uplift of the Tibet Plateau is considered to be the main driving force behind the evolution of the Asian monsoon-arid climate as well as biodiversity in the region. Surface elevation is the intuitive expression of tectonic uplift, but quantitative reconstruction has always been a difficult problem.
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