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Viser: Sedimentary Evolution of the Qinghai-Tibetan Plateau in Cenozoic and Its Response to the Uplift of the Plateau
Sedimentary Evolution of the Qinghai-Tibetan Plateau in Cenozoic and Its Response to the Uplift of the Plateau
Kexin Zhang
(2025)
Springer
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- Hardback: 138 sider
- Udgiver: Springer (Juli 2025)
- ISBN: 9789811065644
Based on highly detailed field investigations and test data from research on 98 different remnant basins, tectonic settings and lithostratigraphic sequences, this book describes the 4-stage evolution of the tectonic lithofacies paleogeography of the Qinghai-Tibetan Plateau, including Paleocene-Eocene, Oligocene, Miocene and Pliocene. It also discusses the contact relationship between the strata, the tectonic-lithofacies paleogeography evolution in the Cenozoic and their response to the tectonic uplift of the plateau. The continuous uplift and intensive intra-continental deformation during each turning point in the plateau divided the originally large sedimentary basins into numerous smaller ones filled with shrank of lacustrine-facies deposition and increased boulderstone accumulation, which indicates a response to the overall uplift of the plateau. Five major uplift events, which happened in 58-53 Ma, 45-30 Ma, 25-20 Ma, 13-7 Ma and since 5 Ma, respectively were identified. The paleogeographic configurations of the Tibetan Plateau turned over during the late Miocene, with high contours in the east during the pre-Miocene switching to the west after the Late Miocene
Introduction.- Tectonic-stratigraphic realm division and basin classification.- Petrological and chronostratigraphic framework.- Paleocene tectonic lithofacies paleogeography of the Tibetan Plateau.- Eocene tectonic lithofacies paleogeography of the Tibetan Plateau.- Oligocene tectonic lithofacies paleogeography of the Tibetan Plateau.- Miocene tectonic lithofacies paleogeography of the Tibetan Plateau.- Pliocene tectonic lithofacies paleogeography of the Tibetan Plateau.- Evolution of Cenozoic tectonic lithofacies paleogeography of the Qinghai-Tibetan Plateau and its response to the uplift of the Plateau.
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