Global cooling and enhanced Eocene Asian mid-latitude interior aridity

Tibetan Plateau uplift has been suggested as the main driving force for mid-latitude Asian inland aridity (AIA) and for deposition of thick aeolian sequences in northern China since the Miocene. However, the relationship between earlier AIA and Tibetan Plateau mountain building is uncertain because...

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Detalles Bibliográficos
Autores principales: Li, J. X., Yue, L. P., Roberts, A. P., Hirt, A. M., Pan, F., Guo, Lin, Xu, Y., Xi, R. G., Guo, Lei, Qiang, X. K., Gai, C. C., Jiang, Z. X., Sun, Z. M., Liu, Q. S.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6072711/
https://www.ncbi.nlm.nih.gov/pubmed/30072688
http://dx.doi.org/10.1038/s41467-018-05415-x

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6072711/
https://www.ncbi.nlm.nih.gov/pubmed/30072688
http://dx.doi.org/10.1038/s41467-018-05415-x

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