Cenozoic double-layered structure in the western Qaidam Basin, northern Tibetan Plateau, China

Author:

Jiang Liwei,Liu Yongjiang,Li Weimin,Yuan Sihua,Yuan Jinglian,Li Sanzhong,Liu Zhihong

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference139 articles.

1. Backthrusts and passive roof duplexes in fold-and-thrust belts The case of Central-Western Sicily based on seismic reflection data;Albanese;Tectonophysics,2012

2. Notes on sedimentary basins in China-Report of the American Sedimentary Basins delegation to the People’s Republic of China;Bally,1986

3. Petrophusical characteristics of the gypsum-salt layer in Qaidam Basin and its influences on tectonic deformation;Bian;Acta Retrolei Sinica,2020

4. Evidence of Miocene crustal shortening in the north Qilian Shan from Cenozoic stratigraphy of the western Hexi Corridor, Gansu Province, China;Bovet;American Journal of Science,2009

5. Growth of the Qaidam Basin during Cenozoic exhumation in the northern Tibetan Plateau: Inferences from depositional patterns and multiproxy detrital provenance signatures;Bush;Lithosphere,2016

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