Mid-Miocene uplift of the northern Qilian Shan as a result of the northward growth of the northern Tibetan Plateau-Reference-Cited by-同舟云学术

Mid-Miocene uplift of the northern Qilian Shan as a result of the northward growth of the northern Tibetan Plateau

Published:2019-01-16 Issue:2 Volume:15 Page:423-432
ISSN:1553-040X
Container-title:Geosphere
language:en
Short-container-title:

Author:

Yu Jingxing¹²,Pang Jianzhang¹,Wang Yizhou¹,Zheng Dewen¹³,Liu Caicai¹,Wang Weitao⁴¹,Li Youjuan¹,Li Chaopeng¹,Xiao Lin¹

Affiliation:

1. State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China

2. Centre for the Observation and Modelling of Earthquakes, Volcanoes and Tectonics (COMET), Department of Earth Sciences, University of Oxford, Oxford OX1 3AN, UK

3. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China

4. School of Earth Sciences and Engineering, Sun Yat-Sen University, Guangzhou 510275, China

Publisher

Geological Society of America

Subject

Stratigraphy,Geology

Link

https://pubs.geoscienceworld.org/gsa/geosphere/article-pdf/15/2/423/4663892/423.pdf

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4. Magnetostratigraphy of Cenozoic deposits in the western Qaidam Basin and its implication for the surface uplift of the northeastern margin of the Tibetan Plateau;Chang;Earth and Planetary Science Letters,2015

5. Magnetochronology of the Yumen conglomerates and multi-pulsed folding and thrusting in the northern Qilianshan;Chen;Quaternary Sciences,2006

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