Crossmark

Clay mineral changes across the Eocene–Oligocene transition in the sedimentary sequence at Xining occurred prior to global cooling

Crossref DOI link: https://doi.org/10.1016/j.palaeo.2014.06.031

Published Print: 2014-10

Update policy: https://doi.org/10.1016/elsevier_cm_policy

Authors

Zhang, Chunxia

Guo, Zhengtang
Funding

Funding for this research was provided by:

Chinese Academy of Sciences (XDB03020500)

National Nature Science Foundation of China (41172159)
License Information

Text and Data Mining valid from 2014-10-01
More Information

This article is maintained by: Elsevier

Article Title: Clay mineral changes across the Eocene–Oligocene transition in the sedimentary sequence at Xining occurred prior to global cooling

Journal Title: Palaeogeography, Palaeoclimatology, Palaeoecology

CrossRef DOI link to publisher maintained version: https://doi.org/10.1016/j.palaeo.2014.06.031

Content Type: article

Copyright: Copyright © 2014 Elsevier B.V. All rights reserved.