Late Miocene Yellow River formation in Qingtongxia area, North China: Detrital zircon and heavy mineral analysis at Niushou Mountain, Ningxia-Reference-Cited by-同舟云学术

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Late Miocene Yellow River formation in Qingtongxia area, North China: Detrital zircon and heavy mineral analysis at Niushou Mountain, Ningxia

Published:2020-09-07 Issue:11 Volume:55 Page:7304-7321
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Bao Guodong¹²^ORCID,Chen Hong¹²^ORCID,Zhao Xitao³

Affiliation:

1. Institute of Geomechanics, Chinese Academy of Geological Sciences Beijing China

2. Key Laboratory of Paleomagnetism and Tectonic Reconstruction Ministry of Natural Resources Beijing China

3. Institute of Geology and Geophysics, Chinese Academy of Science Beijing China

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.3910

Reference117 articles.

1. Evolution of Asian monsoons and phased uplift of the Himalaya–Tibetan plateau since Late Miocene times

2. Correction of common lead in U–Pb analyses that do not report 204Pb

3. Kinematic model of active deformation in central Asia

4. A preliminary study of the Kunlun–Qilian–Qinling suture system;Bian Q. T.;Acta Geoscientia Sinica,2002

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

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2. 黄河形成于何时?;Earth Science-Journal of China University of Geosciences;2024

3. Insights into mineralogical distribution mechanism and environmental significance from geochemical behavior of sediments in the Yellow River Basin, China;Science of The Total Environment;2023-12

4. Meso–Cenozoic Exhumation in the South Qinling Shan (Central China) Recorded by Detrital Apatite Fission-Track Dating of Modern River Sediments;Minerals;2023-10-11

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