Late Oligocene Tectonic Uplift of the East Kunlun Shan: Expansion of the Northeastern Tibetan Plateau-Reference-Cited by-同舟云学术

Late Oligocene Tectonic Uplift of the East Kunlun Shan: Expansion of the Northeastern Tibetan Plateau

Published:2021-01-29 Issue:3 Volume:48 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys Res Lett

Author:

Li Chaopeng¹^ORCID,Zheng Dewen²,Zhou Renjie³^ORCID,Yu Jingxing¹^ORCID,Wang Yizhou¹,Pang Jianzhang¹^ORCID,Wang Ying¹,Hao Yuqi¹,Li Youjuan¹^ORCID

Affiliation:

1. State Key Laboratory of Earthquake Dynamics Institute of Geology China Earthquake Administration Beijing China

2. State Key Laboratory of Isotope Geochemistry Guangzhou Institute of Geochemistry Chinese Academy of Science Guangzhou China

3. School of Earth and Environmental Sciences The University of Queensland St Lucia QLD Australia

Funder

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GL091281

Reference61 articles.

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3. Source to sink relation between the Eastern Kunlun Range and the Qaidam Basin, northern Tibetan Plateau, during the Cenozoic;Cheng F.;Geological Society of America Bulletin,2016

4. Continental collision slowing due to viscous mantle lithosphere rather than topography

5. Early Cenozoic faulting of the northern Tibetan Plateau margin from apatite (U–Th)/He ages

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