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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
Jurassic - Wikipedia
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
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 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
a) Simplified geological map of the Ailaoshan and DayNuiConVoi shear
Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
Late Mesozoic basin evolution in NE China and its surrounding areas, mechanisms of the continental-scale extensional regime in East Asia during the Late Jurassic–Early Cretaceous - ScienceDirect
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
Origin of the largest South American transcontinental water divide
Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
Topographic map of East Asia and major rivers draining southeastern
Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
Reorganization of Asian climate in relation to Tibetan Plateau uplift
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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