Statistics for Millennial-scale climatic change during the last interglacial period: Superparamagnetic sediment proxy from paleosol S1, western Chinese Loess Plateau.
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Millennial-scale climatic change during the last interglacial period: Superparamagnetic sediment proxy from paleosol S1, western Chinese Loess Plateau. | 413 |
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May 2024 | 6 |
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Fang_et_al-1999-Geophysical_Research_Letters.pdf | 245 |
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