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DOI10.1016/j.quascirev.2019.06.011
Formation and evolution of the Holocene massive landslide-dammed lakes in the Jishixia Gorges along the upper Yellow River: No relation to China's Great Flood and the Xia Dynasty
Zhang Y.; Huang C.C.; Shulmeister J.; Guo Y.; Liu T.; Kemp J.; Patton N.R.; Liu L.; Chen Y.; Zhou Q.; Cuan Y.; Zhao H.; Wang N.
发表日期2019
ISSN0277-3791
起始页码267
结束页码280
卷号218
英文摘要The massive Holocene landslide-damming in the Jishixia Gorges along the upper Yellow River was previously suggested to be related to China's Great Flood at 4.20–4.00 ka BP and the initiation of the first dynasty in China: the Xia Dynasty. Here, we present seven sedimentary profiles in the Xunhua Basin and Jishixia Gorges. The lithological, sedimentary and chronological results, including optically stimulated luminescence (OSL) and AMS 14C ages, indicate that there were two separate landslide-dammed lakes rather than one during the Holocene in the Jishixia Gorges. The first lake relates to the Maerpo landslide that occurred at ca. 8.30 ka BP. This lake gradually shallowed and then disappeared by ca. 6.30 ka BP as the landslide dam was slowly incised by the Yellow River. The second Gelongbu landslide occurred at ca. 6.10 ka BP. The consequent lake also gradually shallowed and then disappeared at ca. 5.60 ka BP as the landslide dam was cut through by the Yellow River. Both landslides and their associated lakes preceded The Great Flood in the middle-lower Yellow River by at least 1400 years and preceded the beginning of Xia Dynasty by at least 1600 years. The geomorphic events and therefore unrelated to these historical events. © 2019 Elsevier Ltd
英文关键词China's Great Flood; Jishixia Gorges; Landslide-dammed lakes; Xia Dynasty; Yellow River
语种英语
scopus关键词Floods; Lakes; Lithology; Luminescence; Rivers; Sedimentology; Formation and evolutions; Jishixia Gorges; Landslide-dammed lakes; Lower Yellow River; Optically stimulated luminescence; Upper yellow rivers; Xia Dynasty; Yellow river; Landslides; flood; Holocene; landform evolution; landslide; paleoenvironment; sedimentary sequence; China; Yellow River
来源期刊Quaternary Science Reviews
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/151846
作者单位Shaanxi Key Laboratory of Earth Surface System and Environmental Carrying Capacity, College of Urban and Environmental Sciences, Northwest University, Xi'an, Shaanxi 710127, China; School of Geography and Tourism, Shaanxi Normal University, Xi'an, Shaanxi 710119, China; State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, Shaanxi 710061, China; School of Earth and Environmental Sciences, University of Queensland, St Lucia, Brisbane, Queensland 4072, Australia; Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu, Sichuan 610041, China; Department of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ 85721-0011, United States; Australian Rivers Institute, Griffith University, Nathan, Brisbane, Queensland 4111, Australia; School of Life and Geographic Sciences, Qinghai Normal University, Xining, Qinghai 810008, China
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Zhang Y.,Huang C.C.,Shulmeister J.,et al. Formation and evolution of the Holocene massive landslide-dammed lakes in the Jishixia Gorges along the upper Yellow River: No relation to China's Great Flood and the Xia Dynasty[J],2019,218.
APA Zhang Y..,Huang C.C..,Shulmeister J..,Guo Y..,Liu T..,...&Wang N..(2019).Formation and evolution of the Holocene massive landslide-dammed lakes in the Jishixia Gorges along the upper Yellow River: No relation to China's Great Flood and the Xia Dynasty.Quaternary Science Reviews,218.
MLA Zhang Y.,et al."Formation and evolution of the Holocene massive landslide-dammed lakes in the Jishixia Gorges along the upper Yellow River: No relation to China's Great Flood and the Xia Dynasty".Quaternary Science Reviews 218(2019).
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