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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
Cretaceous Period - Mesozoic, Paleogene, Cenozoic
Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
Geological map of the Markam Basin in south-eastern Tibet. The red star
Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
The topographic evolution of the Tibetan Region as revealed by palaeontology
Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
Geology of the Himalayas - Wikipedia
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
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
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
Minerals, Free Full-Text
Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
Frontiers A Middle to Late Miocene Trans-Andean Portal: Geologic Record in the Tatacoa Desert
Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
Two-phase growth of high topography in eastern Tibet during the Cenozoic
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