Long-lagged (∼19 Myr) response of accelerated river incision to rock uplift on the northern margin of the Tibetan Plateau

Author:

Ye YuhuiORCID,Wu LeiORCID,Cowgill Eric,Tian Yuntao,Lin XiubinORCID,Xiao Ancheng,Chen Hanlin

Funder

National Academy of Sciences

Cyrus Tang Foundation

National Natural Science Foundation of China

Fundamental Research Funds for the Central Universities

National Science Foundation

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference50 articles.

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2. Apatite fission-track records of the tectonic uplift of the central segment of the Kunlun Mountains on the northern margin of the Qinghai-Tibet Plateau;Bai;Geol. China,2003

3. Geodetic evidence for a low slip rate in the Altyn Tagh fault system;Bendick;Nature,2000

4. Cenozoic uplifting and exhumation process of the Altyn Tagh mountains;Chen;Earth Sci. Front.,2006

5. Initial rupture and displacement on the Altyn Tagh fault, northern Tibetan Plateau: constraints based on residual Mesozoic to Cenozoic strata in the western Qaidam Basin;Cheng;Geosphere,2015

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