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Paleoenvironmental changes in the northeastern margin of the Tibetan Plateau since MIS 3: Magnetic evidence from the second terrace of the Yellow River
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DOI码：10.1016/j.catena.2025.109161
发表刊物：Catena
论文类型：文章
卷号：257
页面范围：109161
是否译文：否
收录刊物：SCI
第一作者：赵嘉雯
通讯作者：张玉柱
上一条：The relationship between Holocene environmental evolution and human activities on the Chinese Loess Plateau inferred from an aeolian loess-paleosol profile in the Xitou Ruins
下一条：Formation ages and environmental conditions of paleo-periglacial involutions in the Yellow River source area, northeastern Tibetan Plateau