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- W2283775974 abstract "The uplift history of the Tibetan Plateau remains one of most intriguing and controversial issues in the Cenozoic history of our planet, and has a significant impact on regional and global climate. Here, we report new low-temperature thermochronology apatite and zircon data from the Gangdese batholith in southern Tibet. Thermal history modeling of the data show that the batholith experienced a phase of rapid Early Cenozoic cooling probably associated with exhumation resulting from the initial India-Asia's collision, but possibly also due to postarc volcanic activity in the region. The batholith, then transitioned to low erosion rates (<0.05 mm/yr) between the Middle Eocene and Early Miocene, followed by a renewed episode of cooling commencing in the Early Miocene. Our results indicate that the Gangdese belt, as the southern margin of Eocene Tibetan Plateau, became plateau-like by ∼45 Ma. The later cooling episode from Early Miocene onward, can probably be attributed to incision of the ancestral Yarlung River system, cutting through the Gangdese belt by ∼22 Ma at the latest." @default.
- W2283775974 created "2016-06-24" @default.
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- W2283775974 date "2016-01-01" @default.
- W2283775974 modified "2023-10-13" @default.
- W2283775974 title "Synorogenic morphotectonic evolution of the Gangdese batholith, South Tibet: Insights from low-temperature thermochronology" @default.
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- W2283775974 doi "https://doi.org/10.1002/2015gc006047" @default.
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