Continuity of the Sangdanlin Paleocene section and rejection of a large Greater India in the Early Cretaceous-Reference-Cited by-同舟云学术

Continuity of the Sangdanlin Paleocene section and rejection of a large Greater India in the Early Cretaceous

Published:2024-04-29 Issue:19 Volume:121 Page:
ISSN:0027-8424
Container-title:Proceedings of the National Academy of Sciences
language:en
Short-container-title:Proc. Natl. Acad. Sci. U.S.A.

Author:

Huang Wentao¹^ORCID,Garzanti Eduardo²^ORCID,Moore Theodore C.³^ORCID,Kapp Paul⁴^ORCID,DeCelles Peter G.⁴,Niu Shanshan⁵

Affiliation:

1. State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China

2. Department of Earth and Environmental Sciences, Università di Milano-Bicocca, Milano 20126, Italy

3. Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor, MI 48109-1005

4. Department of Geosciences, University of Arizona, Tucson, AZ 85721

5. North China Electric Power University, Beijing 100096, China

Publisher

Proceedings of the National Academy of Sciences

Link

https://pnas.org/doi/pdf/10.1073/pnas.2402456121

Reference10 articles.

1. Paleocene deep-water sediments and radiolarian faunas: Implications for evolution of Yarlung-Zangbo foreland basin, southern Tibet;Ding L.;Sci. China Earth Sci.,2003

2. Direct stratigraphic dating of India-Asia collision onset at the Selandian (middle Paleocene, 59 ± 1 Ma)

3. Paleocene-Eocene foreland basin evolution in the Himalaya of southern Tibet and Nepal: Implications for the age of initial India-Asia collision

4. Triple-stage India-Asia collision involving arc-continent collision and subsequent two-stage continent-continent collision

5. Strengthening the argument for a large Greater India