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- W2118560742 abstract "The surface uplift of the Tibetan Plateau is the key boundary condition in many Cenozoic geological events ranging from global cooling to changes of Asian environments during Cenozoic. However, poorly constrained timing for the uplift of Tibetan Plateau makes these interpretations highly debatable. Here we report results from sedimentology, detrital zircon U–Pb and Lu–Hf isotopic compositions, and paleomagnetic signatures from both the eastern and western Hoh Xil basins of north-central Tibetan Plateau. Sedimentary lithofacies and facies associations analyzed in the western Hoh Xil basin indicate they were deposited in a braided fluvial system and alluvial fan, similar with the Fenghuoshan Group, eastern Hoh Xil basin. Provenance analyses from conglomerate clast compositions, paleocurrent orientations, and detrital zircon U–Pb and Lu–Hf isotopic compositions document sediments in both western and eastern basins were derived from the Qiangtang and Lhasa blocks. These observations, in combination with comparative paleomagnetic results, imply that Hoh Xil basin was a single, wide basin during Paleogene. The period of Hoh Xil basin deposition was coeval with significant period of the early Cenozoic uplift and erosion of the Qiangtang and Lhasa blocks. These observations not only reinforce the suggestion that the Qiangtang and Lhasa blocks were uplifted during Eocene to form a proto-Tibetan Plateau, but also imply that the proto-Tibet Plateau is vast in areal extent. The large dimension and high elevation of the proto-Tibetan Plateau probably contributed to the global cooling during the early Eocene." @default.
- W2118560742 created "2016-06-24" @default.
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- W2118560742 date "2012-09-01" @default.
- W2118560742 modified "2023-10-03" @default.
- W2118560742 title "The vast proto-Tibetan Plateau: New constraints from Paleogene Hoh Xil Basin" @default.
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- W2118560742 cites W1769330608 @default.
- W2118560742 cites W1871734886 @default.
- W2118560742 cites W1974467019 @default.
- W2118560742 cites W1974623749 @default.
- W2118560742 cites W1976696102 @default.
- W2118560742 cites W1977092507 @default.
- W2118560742 cites W1977938914 @default.
- W2118560742 cites W1985146281 @default.
- W2118560742 cites W1996837794 @default.
- W2118560742 cites W1997816021 @default.
- W2118560742 cites W1999924690 @default.
- W2118560742 cites W2001218033 @default.
- W2118560742 cites W2005769501 @default.
- W2118560742 cites W2011834231 @default.
- W2118560742 cites W2013256761 @default.
- W2118560742 cites W2017477244 @default.
- W2118560742 cites W2018858924 @default.
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- W2118560742 cites W2022859730 @default.
- W2118560742 cites W2024642111 @default.
- W2118560742 cites W2028082622 @default.
- W2118560742 cites W2031763464 @default.
- W2118560742 cites W2032184518 @default.
- W2118560742 cites W2038748953 @default.
- W2118560742 cites W2041774199 @default.
- W2118560742 cites W2048104343 @default.
- W2118560742 cites W2049652180 @default.
- W2118560742 cites W2051273227 @default.
- W2118560742 cites W2052579497 @default.
- W2118560742 cites W2054590577 @default.
- W2118560742 cites W2056983983 @default.
- W2118560742 cites W2067628429 @default.
- W2118560742 cites W2074292075 @default.
- W2118560742 cites W2082181291 @default.
- W2118560742 cites W2085465539 @default.
- W2118560742 cites W2090206242 @default.
- W2118560742 cites W2093114941 @default.
- W2118560742 cites W2094108291 @default.
- W2118560742 cites W2094435009 @default.
- W2118560742 cites W2095800081 @default.
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- W2118560742 cites W2130813033 @default.
- W2118560742 cites W2135640029 @default.
- W2118560742 cites W2136389603 @default.
- W2118560742 cites W2140991916 @default.
- W2118560742 cites W2142833319 @default.
- W2118560742 cites W2148333149 @default.
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- W2118560742 cites W2171150525 @default.
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- W2118560742 doi "https://doi.org/10.1016/j.gr.2011.08.019" @default.
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