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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 23 outubro 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
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
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
Frontiers Late Cenozoic Denudation and Topographic Evolution History of the Lhasa River Drainage in Southern Tibetan Plateau: Insights From Inverse Thermal History Modeling
Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
Frontiers New Paleomagnetic Constraints on the Early Cretaceous Paleolatitude of the Lhasa Terrane (Tibet)
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
Discovery of Late Triassic bivalves from Jurassic deep-water deposits in Riganpeicuo area, Tibet and their geological significance
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
Frontiers An Early Miocene Lowland on the Northeastern Tibetan Plateau
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
Revised chronology of central Tibet uplift (Lunpola Basin)
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
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