Mid-Miocene initiation of the Aimunike-Oulongbuluke Range in the NE Qaidam Basin, implications for the growth of the Tibetan Plateau-Reference-Cited by-同舟云学术

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Mid-Miocene initiation of the Aimunike-Oulongbuluke Range in the NE Qaidam Basin, implications for the growth of the Tibetan Plateau

Published:2019-10-29 Issue:16 Volume:62 Page:2039-2052
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Mao Liguang¹,Wang Liang²,Zhang Junyong³,Fu Suotang⁴,Xiao Ancheng⁵,Liang Xufeng¹

Affiliation:

1. College of Geoscience and Surveying Engineering, China University of Mining & Technology, Beijing, China

2. Unconventional Oil and Gas Resource Center, Shenhua Geological Exploration Co. Ltd, Beijing, China

3. Geological Research Center, BGP Inc., China National Petroleum Corporation, Zhuozhou, China

4. Exploration and Development Research Institute, Qinghai Oilfield Company, PetroChina, Dunhuang, China

5. School of Earth Sciences, Zhejiang University, Hangzhou, China

Funder

National Natural Science Foundation of China

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2019.1683768

Reference66 articles.

1. When and where did India and Asia collide?

2. Himalayan tectonics explained by extrusion of a low-viscosity crustal channel coupled to focused surface denudation

3. Evidence of Miocene crustal shortening in the North Qilian Shan from Cenozoic stratigraphy of the western Hexi Corridor, Gansu Province, China

4. Comparing the November 2002 Denali and November 2001 Kunlun Earthquakes

5. Growth of the Qaidam Basin during Cenozoic exhumation in the northern Tibetan Plateau: Inferences from depositional patterns and multiproxy detrital provenance signatures

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