Confirmation of a Late Miocene Subchron C4n.2n‐1r From the Eastern Qaidam Basin in the NE Tibetan Plateau-Reference-Cited by-同舟云学术

Confirmation of a Late Miocene Subchron C4n.2n‐1r From the Eastern Qaidam Basin in the NE Tibetan Plateau

Published:2019-12 Issue:12 Volume:124 Page:12354-12365
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Gao Peng¹²,Nie Junsheng¹²^ORCID,Li Mingsong³^ORCID,Li Pu¹

Affiliation:

1. Key Laboratory of Western China's Environment System (Ministry of Education), College of Earth and Environmental Sciences Lanzhou University Lanzhou China

2. CAS Center for Excellence in Tibetan Plateau Earth Sciences Chinese Academy of Sciences Beijing China

3. Department of Geosciences Pennsylvania State University University Park PA USA

Funder

National Natural Science Foundation of China

Ministry of Science and Technology of the People's Republic of China

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019JB017936

Reference51 articles.

1. Cyclostratigraphic constraints on the duration of the Datangpo Formation and the onset age of the Nantuo (Marinoan) glaciation in South China

2. Geomagnetic reversals and crustal spreading rates during the Miocene

3. Milankovitch and sub-Milankovitch forcing of the Oxfordian (Late Jurassic) Terres Noires Formation (SE France) and global implications

4. Astronomical calibration of the Toarcian Stage: Implications for sequence stratigraphy and duration of the early Toarcian OAE

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