Holocene climate change in the Maoyaba Basin, western Sichuan Plateau
Objective The Holocene climate of the Tibetan Plateau (TP) is mainly controlled by midlatitude westerlies, the East Asian monsoon, and the Indian monsoon. Previous studies have identified different patterns of Holocene climate change in different regions of the TP. Holocene climate reconstructions f...
Tallennettuna:
| Päätekijät: | , , , |
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| Aineistotyyppi: | Artigo |
| Kieli: | Chinês |
| Julkaistu: |
Editorial Department of Bulletin of Geological Science and Technology
2024-01-01
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| Sarja: | 地质科技通报 |
| Aiheet: | |
| Linkit: | https://dzkjqb.cug.edu.cn/en/article/doi/10.19509/j.cnki.dzkq.tb20220278 |
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