Differences in east-west thermo-rheological structure and lithospheric deformation in the Qaidam Basin, Northern Tibetan Plateau, China-Reference-Cited by-同舟云学术

Differences in east-west thermo-rheological structure and lithospheric deformation in the Qaidam Basin, Northern Tibetan Plateau, China

Published:2021-03-08 Issue: Volume: Page:1-20
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Li Chaoyang¹,Jiang Xiaodian²³,Gong Wei²³,Zhou Haiting⁴,Yang Kai⁵

Affiliation:

1. School of Ocean Science and Technology, Dalian University of Technology, Panjin, China

2. Key Lab of Submarine Geosciences and Prospecting Techniques, Ministry of Education, and College of Marine Geosciences, Ocean University of China, Qingdao, China

3. Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao, China

4. Exploration and Development Institute of Shengli Oilfield, Dongying, China

5. Xinjiang Uygur Autonomous Region Committee of the Communist Youth League, Urumqi, China

Funder

National Natural Science Foundation of China

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2021.1894610

Reference99 articles.

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2. Cenozoic sediment flux in the Qaidam Basin, northern Tibetan Plateau, and implications with regional tectonics and climate

3. Spatial variations of flexure parameters over the Tibet–Quinghai plateau

4. Lithosphere density model in Italy: no hint for slab pull

5. Empirical Relations between Elastic Wavespeeds and Density in the Earth's Crust

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