Constraints on the early uplift history of the Tibetan Plateau

By Chengshan Wang, Xixi Zhao, Zhifei Liu, P. Lippert, S. Graham, R. Coe, H. Yi, Lidong Zhu, Shunlin Liu, Yalin Li. Proceedings of the National Academy of Sciences of the United States of America, 2008

803 citations recorded by the source corpus.

Subfields: Atmospheric Science, Geophysics

View Paper: https://www.semanticscholar.org/paper/36122b6a3102fff4b2c375450bee86e847b16d78

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In Atmospheric Science

1. S. Pauls
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1. Hailiang Dong
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Citations in the corpus

• Phylogeography of regional fauna on the Tibetan Plateau: A review (2009, background): “[21] based on geological and geophysical evidence supports the idea that the central plateau (the Lhasa and southern Qiangtang Terranes, namely, the proto-Tibetan Plateau) was elevated 40 Myr ago, and the south and north of the protoplateau gained the present elevation significantly later.”
• The role of the uplift of the Qinghai‐Tibetan Plateau for the evolution of Tibetan biotas (2015, background): “Simultaneously, significant orogeny of the Himalayas (up to an elevation comparable to present day) is likely to have happened in the same timeframe (Tapponnier et al., 2001; Wang et al., 2008; Zhang et al., 2013a), though the onset of the Himalayan orogeny (generating some punctual high altitudes) ”
• Greater India Basin hypothesis and a two-stage Cenozoic collision between India and Asia (2012, background): “This collision led to orogeny (14, 45), but was followed by ongoing oceanic subduction of the GIB.”
• Evolutionary origin of species diversity on the Qinghai–Tibet Plateau (2021, background): “For example, the inferred uplift in one site (one mountain or one relatively small region) based on certain evidence was mistakenly used or expressed to represent the whole QTPsl or a larger region (Tapponnier et al., 2001; Wang et al., 2008; Renner, 2016; Su et al., 2019a, 2019b).”
• Plant phylogeography in arid Northwest China: Retrospectives and perspectives (2015, background): “By the earlyMiocene, central parts of the QTP may have uplifted to present heights (Wang et al., 2008; Wu et al., 2008), and long-term dust deposition in the Loess Plateau and Dzungarian Basin were established (Guo et al.”