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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
Pulsed rise and growth of the Tibetan Plateau to its northern margin since ca. 30 Ma
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
Geology of the Himalayas - Wikipedia
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
Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
Tertiary Period, Events, Climate, & Organisms
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
Two-phase growth of high topography in eastern Tibet during the 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
A climate-driven transcontinental drainage system in the southeast Tibetan Plateau during the Early Cretaceous - ScienceDirect
Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
Mio-Pliocene piracy, relict landscape and drainage reorganization in the Namcha Barwa syntaxis zone of eastern Himalaya
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
Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
The Geological Evolution of the Tibetan Plateau
Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
Cretaceous source to sink system reconstruction of northeastern Asian continental margin: Insight from integrated detrital geochronology in NE China - ScienceDirect
Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
Cretaceous source to sink system reconstruction of northeastern Asian continental margin: Insight from integrated detrital geochronology in NE China - ScienceDirect
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