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

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Last updated 02 abril 2025
Existence of a continental-scale river system in eastern Tibet during the  late Cretaceous–early Palaeogene
Existence of a continental-scale river system in eastern Tibet during the  late Cretaceous–early Palaeogene
Middle–Late Cenozoic Stepwise Deformation Propagation in Eastern Tibet - Tao - 2023 - Geophysical Research Letters - Wiley Online Library
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
Full article: Buried Jurassic rift system in the middle segment of the northern Qaidam Basin: Implications for Mesozoic landforms of the northern Tibetan Plateau
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
Cratonic basins as effective sediment barriers in continent-scale sediment routing systems of Paleozoic North America
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
Middle–Late Cenozoic Stepwise Deformation Propagation in Eastern Tibet - Tao - 2023 - Geophysical Research Letters - Wiley Online Library
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
Simplified paleogeographic maps showing the development of the Red
Existence of a continental-scale river system in eastern Tibet during the  late Cretaceous–early Palaeogene
Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene

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