Paleoclimate evolution and aridification mechanism of the eastern Tethys during the Callovian–Oxfordian: evidence from geochemical records of the Qiangtang Basin, Tibetan Plateau
Crossref DOI link: https://doi.org/10.1007/s11631-021-00458-2
Published Online: 2021-02-24
Published Print: 2021-04
Update policy: https://doi.org/10.1007/springer_crossmark_policy
Zeng, Yongyao http://orcid.org/0000-0002-5074-6797
Gao, Lei
Zhao, Wenqing
Funding for this research was provided by:
National Basic Research Program of China (2011CB403003)
Text and Data Mining valid from 2021-02-24
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Article History
Received: 12 January 2021
Revised: 12 January 2021
Accepted: 2 February 2021
First Online: 24 February 2021