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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 Plateau
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DOI码：10.3389/feart.2023.1144283
发表刊物：Frontiers in Earth Science
论文类型：期刊论文
卷号：11
页面范围：1144283
是否译文：否
第一作者：王硕
通讯作者：张玉柱
上一条：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, China
下一条：Sedimentary records and chronology of the late Pleistocene overbank flooding in the Yellow River source area, NE Tibetan Plateau