Stepwise increased spatial provenance contrast on the Chinese Loess Plateau over late Miocene-Pleistocene
The formation of the Chinese Loess Plateau resulted from a combination of surface processes rather than from aridification of the Asian interior alone, according to zircon U-Pb geochronological analysis
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| Asıl Yazarlar: | , , , , , , |
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| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
Nature Portfolio
2023-03-01
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| Seri Bilgileri: | Communications Earth & Environment |
| Online Erişim: | https://doi.org/10.1038/s43247-023-00721-9 |
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