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Existence of a continental-scale river system in eastern Tibet during the late Cretaceous–early Palaeogene
The establishment of continental-scale drainage systems on Earth is largely controlled by topography related to plate boundary deformation and buoyant mantle. Drainage patterns of the great rivers in Asia are thought to be highly dynamic during the Cenozoic collision of India and Eurasia, but the dr...
Autores principales: | , , , , , , , , , , , , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2021
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8668954/ https://www.ncbi.nlm.nih.gov/pubmed/34903729 http://dx.doi.org/10.1038/s41467-021-27587-9 |