【作者单位】1State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China;2State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences (NIGLAS), Nanjing 210008, China;3Kunming Engineering Corporation Limited, Kunming 650033, China;4Department of Archaeology, Jahangirnagar University, Dhaka 1342, Bangladesh;5Institute of Nihewan Archaeology, Hebei Normal University, Shijiazhuang 050024, Hebei Province, China;6State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510630, China;7China University of Geosciences, 100083, Beijing, China;8Key Laboratory for Earth Surface Processes, Department of Geography, Peking University, Beijing 100871, China;9Key Laboratory of Cosmic Rays of Ministry of Education of China, Tibet University, Lhasa, 850000, China
【年份】2023
【卷号】Vol.622
【页码】118387
【ISSN】0012-821X
【摘要】 Fluvial sediment fingerprinting employs various methods, directly link sink and source. However, the identification and quantification of the transformation that sediments experience during fluvial transport remain unclear. The luminescence propertie...
