Tectonic and orbital forcing of the South Asian monsoon in central Tibet during the late Oligocene

The modern pattern of the Asian monsoon is thought to have formed around the Oligocene/Miocene transition and is generally attributed to Himalaya–Tibetan Plateau (H–TP) uplift. However, the timing of the ancient Asian monsoon over the TP and its response to astronomical forcing and TP uplift remains...

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Detalles Bibliográficos
Autores principales: Jin, Chun-Sheng, Xu, Deke, Li, Mingsong, Hu, Pengxiang, Jiang, Zhaoxia, Liu, Jianxing, Miao, Yunfa, Wu, Fuli, Liang, Wentian, Zhang, Qiang, Su, Bai, Liu, Qingsong, Zhang, Ran, Sun, Jimin
Formato: Online Artículo Texto
Lenguaje:English
Publicado: National Academy of Sciences 2023
Materias:
Physical Sciences
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10104490/
https://www.ncbi.nlm.nih.gov/pubmed/37011203
http://dx.doi.org/10.1073/pnas.2214558120

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10104490/
https://www.ncbi.nlm.nih.gov/pubmed/37011203
http://dx.doi.org/10.1073/pnas.2214558120

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