Plio-Pleistocene drainage reorganization in the middle Yellow River of China, revealed by provenance and paleocurrent analysis of fluvial sediments-Reference-Cited by-同舟云学术

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Plio-Pleistocene drainage reorganization in the middle Yellow River of China, revealed by provenance and paleocurrent analysis of fluvial sediments

Published:2024-06 Issue: Volume:454 Page:109177
ISSN:0169-555X
Container-title:Geomorphology
language:en
Short-container-title:Geomorphology

Author:

Li Menghao,Hu Zhenbo,Wang Ping,Pan Baotian,Bridgland David,Mo Qinhong,Li Xiaohua,Dong Zijuan,Zhong Meiling,Pan Renzhe,Li Ningyi

Funder

Fundamental Research Funds for the Central Universities

National Natural Science Foundation of China

State Administration of Foreign Experts Affairs

Publisher

Elsevier BV

Reference64 articles.

1. Global warming-induced Asian hydrological climate transition across the Miocene-Pliocene boundary;Ao;Nat. Commun.,2021

2. The uplift history of the Arabian Plateau as inferred from geomorphologic analysis of its northwestern edge;Bar;Tectonophysics,2016

3. Neogene global climate change and East Asian dust sources: combined rutile geochemistry and zircon U-Pb analysis from the northern Chinese Loess Plateau;Bohm;Glob. Planet. Chang.,2023

4. Strath terraces of Jinshaan Canyon, Yellow River, and Quaternary tectonic movements of the Ordos Plateau, North China;Cheng;Terra Nova,2002

5. Rapid fluvial incision along the Yellow River during headward basin integration;Craddock;Nat. Geosci.,2010

Cited by 1 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. How Was the Late Neogene Red Clay Formed in the Ordos Plateau (Northwest China)?;Minerals;2024-05-23

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