Aeolian activity in the Yarlung Zangbo River Basin, southern Tibetan Plateau, began at 584 ka: implications for the glaciation of the Tibetan PlateauQUATERNARY SCIENCE REVIEWSIF3.32024-08-012PRE
Aeolian process and climatic changes in loess records from the eastern Tibetan Plateau: Implications for paleoenvironmental dynamics since MIS 3CATENAIF5.72023-10-015OAAI
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HIRM variation in the Ganzi loess of the eastern Tibetan Plateau since the last interglacial period and its paleotemperature implications for the source regionGONDWANA RESEARCHIF8.62022-01-019PRE
Comparisons of topsoil geochemical elements from Northwest China and eastern Tibetan Plateau identify the plateau interior as Tibetan dust sourceSCIENCE OF THE TOTAL ENVIRONMENTIF82021-12-0132PRE
Holocene moisture evolution and its response to atmospheric circulation recorded by aeolian deposits in the southern Tibetan PlateauQUATERNARY SCIENCE REVIEWSIF3.32021-10-0127PREAI
Chronology and dust mass accumulation history of the Wenchuan loess on eastern Tibetan Plateau since the last glacialAEOLIAN RESEARCHIF3.42021-09-0114PRE
Evolution of Near-Surface Wind Strength in Northeastern Arid Central Asia During the HolocenePALEOCEANOGRAPHY AND PALEOCLIMATOLOGYIF3.22021-02-1814PRE
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