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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
- 金瑶.Formation ages and environmental conditions of paleo-periglacial involutions in the Yellow River source area, northeastern Tibetan PlateauPalaeogeography, Palaeoclimatology, Palaeoecology,2024,659(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
- 朱艳.Sedimentary records and chronology of the late Pleistocene overbank flooding in the Yellow River source area, NE Tibetan PlateauFrontiers in Earth Science,2022,10(1021106-1021106
- 肖奇立.Paleochannel of the Yellow River within the Zoige Basin and its environmental significance on the NE Tibetan PlateauScience of the Total Environment,2022,853(158242-158242
- 贾雅娜.Weathering and pedogenesis of the late Pleistocene and Holocene aeolian loess-paleosol sections in the Yellow River source area, NE Tibetan PlateauPalaeogeography, Palaeoclimatology, Palaeoecology,2022,600):111065-111065
- 吴萌蕾.Heavy metal pollution from copper smelting during the Shang Dynasty at the Laoniupo site in the Bahe River valley, Guanzhong Basin, ChinaJournal of Geographical Sciences,2021,31(11):1675-1693