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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
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
Remote Sensing, Free Full-Text
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
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
PDF) 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
Geodynamic evolution of North Tibet from Permian to Tertiary (modified
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
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
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
a) The distribution of the representative potash deposits in the
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
Revised chronology of central Tibet uplift (Lunpola Basin)
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
A) Compiled stratigraphic columns across the Chuxiong, Xichang and
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