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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Vydáno v:Nat Commun
Hlavní autoři: 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.
Médium: Artigo
Jazyk:Inglês
Vydáno: Nature Publishing Group UK 2018
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On-line přístup:https://ncbi.nlm.nih.gov/pmc/articles/PMC6072711/
https://ncbi.nlm.nih.gov/pubmed/30072688
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-05415-x
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