Transient Fluvial Incision in the Central Segment of the Lancang River Orogenic Belt,Yunnan Province,SW China

摘要

Objective Geomorphology has played a central role in the study of active orogenic belts.Extensive tectonic deformation associated with the collision of the Indian and Eurasian plates has occurred in the southeastern margin of the Tibetan Plateau,particularly along the Lancang River Orogenic Belt(LROB)and the Lancang River Fault.