Spatial and temporal pattern of erosion in the Three Rivers Region, southeastern Tibet
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文摘

54 new thermochronometric ages from southeastern Tibet are presented.

Inferred erosion rates decrease from west to east.

Inferred erosion rates show spatial and temporal variations from south-to-north.

Locus of fast erosion migrates northwards along the Salween and Mekong.

An active coupling between river incision and tectonics is inferred.

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