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- Comment on “ Outburst flood at 1920 BCE supports historicity of China’s Great Flood and the Xia dynasty”Science,2017,355/1382d
- 张玉柱.Paleoclimatic evolution since the Late Pleistocene in western Central Asia and its response to mid-latitude westerlies and low-latitude high pressure: insights from aeolian loess-paleosol sections in the Surkhandarya River BasinQuaternary Science Reviews,2025,368(109553
- 曹鹏鹏.Evolutionary history of a paleo-oxbow lake in the Yellow River within the Zoige Basin, NE Tibetan PlateauQuaternary International,2025,745(109938
- 李孟停.The relationship between Holocene environmental evolution and human activities on the Chinese Loess Plateau inferred from an aeolian loess-paleosol profile in the Xitou RuinsCatena,2025,258(109271
- 赵嘉雯.Paleoenvironmental changes in the northeastern margin of the Tibetan Plateau since MIS 3: Magnetic evidence from the second terrace of the Yellow RiverCatena,2025,257(109161
- 金瑶.Formation ages and environmental conditions of paleo-periglacial involutions in the Yellow River source area, northeastern Tibetan PlateauPalaeogeography, Palaeoclimatology, Palaeoecology,2025,659(112659
- 陈豆.Micromorphological characteristics and environmental significance of the Holocene aeolian loess-paleosol section in the Zoige BasinCatena,2024,246(108415-108415
- 朱艳.Weathering and pedogenesis of the Holocene aeolian loess-paleosol sections in the Guanzhong Basin on the Chinese Loess PlateauJournal of Asian Earth Sciences,2024,276(106334-106334
- 张玉柱.Char and soot records of the Holocene fire history and its implications for climate-vegetation change and human activities within the Guanzhong Basin, southern Loess Plateau, ChinaScience of the Total Environment,2024,911(168564-168564
- 王硕.Geochemistry of a paleo-oxbow lake sediments and its implications for the late Holocene extreme overbank flooding history of the Yellow River within the Zoige Basin, NE Tibetan PlateauFrontiers in Earth Science,2023,11(1144283-1144283