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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 27 novembro 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
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
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
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 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 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
Mid-Cretaceous drainage reorganization and exorheic to endorheic transition in Southeast Tibet - ScienceDirect
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
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
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
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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
PDF) Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
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