Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
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Last updated 11 março 2025


PDF) 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

Cretaceous source to sink system reconstruction of northeastern Asian continental margin: Insight from integrated detrital geochronology in NE China - ScienceDirect

Minerals, Free Full-Text

Cratonic basins as effective sediment barriers in continent-scale sediment routing systems of Paleozoic North America

Palaeodrainage evolution of the large rivers of East Asia, and Himalayan- Tibet tectonics - ScienceDirect

Carboniferous–Permian Coaly Source Rock Formation in North China: Implications from Geochemical Characteristics and Depositional Environments

A climate-driven transcontinental drainage system in the southeast Tibetan Plateau during the Early Cretaceous - ScienceDirect

Sedimentary provenance perspectives on the evolution of the major rivers draining the eastern Tibetan Plateau - ScienceDirect

a) Major rivers draining southeastern Tibet and river sediment

a) The distribution of the representative potash deposits in the

Tertiary Period, Events, Climate, & Organisms
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