Late Cenozoic geomorphic evolution in the northeastern Tibetan Plateau: Constraints on U-Pb age spectra of detrital zircons in the Wuwei Basin, NW China

Author:

Zhao Zixian,Shi Wei,Yang Yong

Funder

National Natural Science Foundation of China

China Geological Survey, Ministry of Natural Resources

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference115 articles.

1. Surface tracks and slip rate of the fault along the southern margin of the Wuwei Basin in the Late Quaternary;Ai;Seismol. Geol.,2017

2. An immediate response to the Indian-Eurasian collision along the northeastern Tibetan Plateau: evidence from apatite fission track analysis in the Kuantan Shan-Hei Shan;An;Tectonophysics,2020

3. Evolution of Asian monsoons and phased uplift of the HimalayaeTibetan plateau since Late Miocene times;An;Nature,2001

4. Late Cenozoic cooling favored glacial over tectonic controls on sediment supply to the western Gulf of Mexico;Angela;Geology,2018

5. Geology of the Haiyuan Fault zone, Ningxia-Hui Autonomous Region, China, and its relation to the evolution of the northeastern margin of the Tibetan Plateau;Burchfiel;Tectonics,1991

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