Large-scale drainage capture and surface uplift in eastern Tibet-SW China before 24 Ma inferred from sediments of the Hanoi Basin, Vietnam
Current models of drainage evolution suggest that the non‐dendritic patterns seen in rivers in SE Asia reflect progressive capture of headwaters away from the Red River during and as a result of surface uplift of Eastern Asia. Mass balancing of eroded and deposited rock volumes demonstrates that the...
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Veröffentlicht in: | Geophysical research letters 2006-10, Vol.33 (19), p.n/a |
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