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- W2531174536 abstract "Abstract A large body of evidence suggests that there were extensive coastal mountains along the East Asian margin during the Late Cretaceous. However, current knowledge of the paleo-mountains — the period, range, and elevation — is limited. Therefore, direct paleoaltimetry is needed to validate and evaluate the paleo-mountains in East Asia. Our study area is Jiaolai Basin, which is located at the East Asian continental margin. We estimate the paleoelevation of Jiaolai Basin during the Late Cretaceous using carbonate clumped isotope paleothermometry. After correcting for seasonal preference, latitudinal difference, and secular climate change, we conclude that the paleoelevation of Jiaolai Basin was almost certainly ≥2.0 km at ∼80 Ma. Combined with the evidence from stratigraphy, paleogeography, and paleoclimatology, our results suggest that the existence of coastal mountains along East Asia during the Late Cretaceous is likely and the model of Okhotomorsk–East Asia collision is preferred." @default.
- W2531174536 created "2016-10-21" @default.
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- W2531174536 date "2016-12-01" @default.
- W2531174536 modified "2023-10-17" @default.
- W2531174536 title "High elevation of Jiaolai Basin during the Late Cretaceous: Implication for the coastal mountains along the East Asian margin" @default.
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- W2531174536 doi "https://doi.org/10.1016/j.epsl.2016.09.034" @default.
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