Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene

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Existence of a continental-scale river system in eastern Tibet during the  late Cretaceous–early Palaeogene
Sedimentary provenance perspectives on the evolution of the major rivers draining the eastern Tibetan Plateau - ScienceDirect
Existence of a continental-scale river system in eastern Tibet during the  late Cretaceous–early Palaeogene
Frontiers Topographic Response of Hinterland Basins in Tibet to the India–Asia Convergence: 3D Thermo-Mechanical Modeling
Existence of a continental-scale river system in eastern Tibet during the  late Cretaceous–early Palaeogene
Minerals, Free Full-Text
Existence of a continental-scale river system in eastern Tibet during the  late Cretaceous–early Palaeogene
Provenance of Late Cretaceous accretionary complex within the Yarlung–Zangpo suture zone, Bainang, southern Tibet: Implications for the subduction–accretion of the Neo-Tethyan ocean - ScienceDirect
Existence of a continental-scale river system in eastern Tibet during the  late Cretaceous–early Palaeogene
Palaeodrainage evolution of the large rivers of East Asia, and Himalayan- Tibet tectonics - ScienceDirect
Existence of a continental-scale river system in eastern Tibet during the  late Cretaceous–early Palaeogene
Palaeoenvironmental changes in Eocene Tibetan lake systems traced by geochemistry, sedimentology and palynofacies - ScienceDirect
Existence of a continental-scale river system in eastern Tibet during the  late Cretaceous–early Palaeogene
Minerals, Free Full-Text
Existence of a continental-scale river system in eastern Tibet during the  late Cretaceous–early Palaeogene
Palaeodrainage evolution of the large rivers of East Asia, and Himalayan- Tibet tectonics - ScienceDirect
Existence of a continental-scale river system in eastern Tibet during the  late Cretaceous–early Palaeogene
The rise and demise of the Paleogene Central Tibetan Valley
Existence of a continental-scale river system in eastern Tibet during the  late Cretaceous–early Palaeogene
Simplified paleogeographic maps showing the development of the Red
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