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

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Last updated 18 junho 2024
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
Fault systems impede incision of the Yarlung river into 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
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
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
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
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
Frontiers Topographic Response of Hinterland Basins in Tibet to the India–Asia Convergence: 3D Thermo-Mechanical Modeling
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
The topographic evolution of the Tibetan Region as revealed by palaeontology
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