Detrital zircon evidence for the ternary sources of the Chinese Loess Plateau

Detrital zircon evidence for the ternary sources of the Chinese Loess Plateau Journal of Asian Earth Sciences 155 (2018) 21–34 Contents lists available at ScienceDirect Journal of Asian Earth Sciences journal homepage: www.elsevier.com/locate/jseaes Full length article a,b, a,b c d e Jimin Sun , Zhongli Ding , Xiaoping Xia , Min Sun , Brian F. Windley Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, P.O. Box 9825, Beijing 100029, China University of Chinese Academy of Sciences, China Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, China Department of Earth Sciences, The University of Hongkong, HK, China Department of Geology, University of Leicester, Leicester LEI 7RH, UK ARTICLE I NFO ABSTRACT Keywords: The provenance of Chinese loess is fundamental for understanding its origin, transportation and climatic sig- Provenance nificance. In this paper, eight samples were collected for detrital zircon age analysis, five from different deserts, Loess Plateau and three from the Jingbian Section in the northern Chinese Loess Plateau, covering an age range of Detrital zircon age 2.6–0.03 Ma. The new results, integrated with knowledge of relevant topography and wind patterns, demon- Mountain erosion strate that the age spectra of the detrital zircons in the loess are different from those of the sands http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Journal of Asian Earth Sciences Elsevier

Detrital zircon evidence for the ternary sources of the Chinese Loess Plateau

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Publisher
Elsevier
Copyright
Copyright © 2017 Elsevier Ltd
ISSN
1367-9120
eISSN
1878-5786
D.O.I.
10.1016/j.jseaes.2017.10.012
Publisher site
See Article on Publisher Site

Abstract

Journal of Asian Earth Sciences 155 (2018) 21–34 Contents lists available at ScienceDirect Journal of Asian Earth Sciences journal homepage: www.elsevier.com/locate/jseaes Full length article a,b, a,b c d e Jimin Sun , Zhongli Ding , Xiaoping Xia , Min Sun , Brian F. Windley Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, P.O. Box 9825, Beijing 100029, China University of Chinese Academy of Sciences, China Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, China Department of Earth Sciences, The University of Hongkong, HK, China Department of Geology, University of Leicester, Leicester LEI 7RH, UK ARTICLE I NFO ABSTRACT Keywords: The provenance of Chinese loess is fundamental for understanding its origin, transportation and climatic sig- Provenance nificance. In this paper, eight samples were collected for detrital zircon age analysis, five from different deserts, Loess Plateau and three from the Jingbian Section in the northern Chinese Loess Plateau, covering an age range of Detrital zircon age 2.6–0.03 Ma. The new results, integrated with knowledge of relevant topography and wind patterns, demon- Mountain erosion strate that the age spectra of the detrital zircons in the loess are different from those of the sands

Journal

Journal of Asian Earth SciencesElsevier

Published: Apr 15, 2018

References

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