Crossmark

On the timing and forcing mechanism of a mid-Miocene arid climate transition at the NE margins of the Tibetan Plateau: stratigraphic and sedimentologic evidence from the Sikouzi Section

Crossref DOI link: https://doi.org/10.1007/s00531-015-1213-z

Published Online: 2015-06-16

Published Print: 2016-04

Update policy: https://doi.org/10.1007/springer_crossmark_policy

Authors

Lin, Xiubin

Wyrwoll, Karl-Heinz

Chen, Hanlin

Cheng, Xiaogan
Funding

Funding for this research was provided by:

National Natural Science Foundation of China (41102128, 41330207, 41272231, 41472181)

National S&T Major Project (2011ZX05009-001)

Fundamental Research Funds for the Central Universities (2014FZA3007, 2015QNA3015)

Open Fund of Key Laboratory of Submarine Geosciences, SOA
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