Glacier-Induced Alluvial Fan Development on the Northeast Tibetan Plateau Since the Late Pleistocene

The origin of alluvial fans at drainage basin or margins of arid sedimentary basin on the northeastern Tibetan Plateau (NETP) are still disputed. Extensive alluvial fans had developed in the mountain-basin systems of this region during the Late Pleistocene. Based on geomorphic/stratigraphic studies and the optically stimulated luminescence (OSL) chronology, we investigated numerous alluvial sequences in the drainage basin of the coupled mountain-basin system on the NETP. Sedimentologic analyses showed that these alluvial sediments mainly comprise crudely meter and decimeter beds of fanglomerate and sandy lenticles, which occasionally contain boulders in the thinner layers. OSL dating results showed that the alluvial sediments were mainly developed during the late MIS 5, MIS3, and Last Glaciation and Deglaciation (maximum aggradations), while little had occurred during early Holocene. Comparing our ages and their probability density curves with that of glacial advances from northeastern/eastern TP, the good consistency of both records during different stages since late Pleistocene suggested that the development of alluvial fans was driven by glacier activities, which yielded abundant outwash and fed alluvial aggradations. Based on this finding together with results of previous studies, we argued that the dynamics of alluvial geomorphic processes had a paleoclimatic origin rather than surface uplifts. Further studies indicated that the precipitation of glaciations originated from ISM northward intrusion during the late MIS 5, MIS 3, and Holocene. However, it was mainly influenced by Westerlies during the Last Glaciation and Deglaciation. Therefore, the development of alluvial fans on the NETP represents coupling signals of ISM and Westerlies on the interglacial-glacial cycle timescales. The coupling evolution of glacier activities and alluvial aggradations in the drainage basins of mountain-basin systems on the NETP offer a model for assessing the linkages between regional geomorphic processes and atmospheric circulations at hemispheric scales.