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Millennial‐scale climatic change during the Last Interglacial Period: Superparamagnetic sediment proxy from Paleosol S1, western Chinese Loess Plateau

机译：末次间冰期的千年尺度气候变化：中国西部黄土高原古土壤s1的超顺磁性沉积物代谢

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Fang, Xiao‐min; Ji‐jun, Li; Banerjee, Subir K.; Jackson, Mike; Oches, Eric A.; Van Der Voo, Rob;
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年度 1999
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1. Millennial-scale climatic change during the last interglacial period: superparamagnetic sediment proxy from paleosol S1, western Chinese loess plateau [J] . Fang Xiao-Min, Banerjee Subir K., Jackson Mike, Geophysical Research Letters . 1999,第16期

机译：最后一个冰期间的千年尺度气候变化：中国西部黄土高原古土壤S1的超顺磁性沉积物代表
2. Vegetation and climate changes during three interglacial periods represented in the Luochuan loess-paleosol section, on the Chinese Loess Plateau [J] . Maotang Cai, Mingjian Wei, Dainan Xu, Quaternary International . 2013,第maya16期

机译：黄土高原洛川黄土古土壤剖面三个间冰期的植被与气候变化
3. Spatiotemporal variations of Zr/Rb ratio in three last interglacial paleosol profiles across the Chinese Loess Plateau and its implications for climatic interpretation [J] . WANG HaiBin, LIU LianYou, FENG ZhaoDong 中国科学通报：英文版 . 2008,第009期

机译：黄土高原中最后三个冰间古土壤剖面中Zr / Rb比的时空变化及其对气候解释的影响
4. Changes in sand content of loess along a transect of western chinese loess plateau and implications for desert evolution [C] . Shujian Xu, Baotian Pan Geoscience and Remote Sensing Symposium, 2005. IGARSS '05. Proceedings. 2005 IEEE International . 2005

机译：中国西部黄土高原样带黄土含沙量变化及其对沙漠演变的启示
5. Stratigraphy and palaeoclimatology of loess of the Loess Plateau, China during the last interglacial-glacial cycle. [D] . Rokosh, Charles Dean. 2001

机译：黄土高原上一次冰河-冰川间期的地层学和古气候学
6. Tetraether biomarker records from a loess-paleosol sequence in the western Chinese Loess Plateau [O] . Guodong Jia, Zhiguo Rao, Jie Zhang, 2013

机译：黄土高原西部黄土古土壤序列中的四醚生物标志物记录
7. Millennial-scale climatic change during the last interglacial period: Superparamagnetic sediment proxy from paleosol S1, western Chinese Loess Plateau. [O] . Fang, Xiaomin, Li, J.-J., Banerjee, Subir, 1999

机译：最后一个冰期间的千年尺度气候变化：来自中国西部黄土高原古土壤S1的超顺磁性沉积物替代物。

Millennial‐scale climatic change during the Last Interglacial Period: Superparamagnetic sediment proxy from Paleosol S1, western Chinese Loess Plateau

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