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How did river drainage systems in southeastern Tibet evolve during the Cenozoic?
Recent provenance work on the Yanyuan Basin offers the clearest record yet of how the upper Yangtze drainage reorganised through the Cenozoic.
Detrital rutile U–Pb and zircon fission-track dating reconstruct a Paleo-Yalong River that flowed southward through the basin 1 — unlike the modern Yalong, which skirts it entirely. In the Pliocene, the catchment expanded eastward 1 2.
SOURCES · 2 PAPERS
1
Drainage Pattern Changes in Southeastern Tibet Inferred from Eocene–Modern Sediment Provenance
Xilin Sun et al.
2
Cenozoic Tectonic Evolution of the Yanyuan Basin
Wei Chen et al.
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