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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 17 maio 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
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Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
Jurassic Evolution of the Dunhuang Basin and Its Implications for the Early History of the Altyn Tagh Fault, Northeast Tibet Plateau - Dai - 2023 - Tectonics - Wiley Online Library
Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
Pulsed rise and growth of the Tibetan Plateau to its northern margin since ca. 30 Ma
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
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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
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Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
Minerals, Free Full-Text
Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
Minerals, Free Full-Text
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
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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
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