Atmospheric circulation in western China significantly affects the inland climate of Asia. Constraining the provenance of eolian sequences can provide robust evidence for dust-transport pathways, and thus the evolution of paleo-atmospheric circulation. Western China has been dominated by the westerly wind regime since the late Oligocene, as demonstrated by provenance studies of eolian deposits. However, the wind regime responsible for the accumulation of eolian deposits during the Eocene is unclear due to a lack of corresponding provenance studies. Here, we present the first provenance analysis for an Eocene (ca. 51−40 Ma) eolian Red Clay sequence in the Xishuigou Formation of the Xorkol Basin in western China, based on multiproxy geochemical and geochronological data. Comparison of zircon U−Pb ages from the Xishuigou sequence with ages from potential source regions reveals that the northern piedmont of the West Kunlun Range was a persistent source, although sediments from the nearby Altun-Xorkol region were an important dust source for the lower part of the Xishuigou sequence which were deposited between ca. 51 Ma and 46.5 Ma. These results reveal that the westerly dust-transport pattern has been dominant in western China since at least ca. 51 Ma. The similarity of provenance between the Eocene Red Clay of the Xishuigou Formation and the Neogene eolian sequence of the overlying Caihonggou Formation in the same area implies that this dust-transport pattern was stable from the Eocene to the Neogene, despite dramatic changes in paleogeography, paleotopography, and global climate.
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Research Article|
January 11, 2023
Provenance of eolian deposits in the Xorkol Basin: Implications for Eocene dust-transport pattern in western China
Feng Pan;
Feng Pan
1
Research Center for Orogenic Geology, Xi’an Center of China Geological Survey, Xi’an 710054, China2
State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi’an 710069, China
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Jianxing Li;
Jianxing Li
3
Cheng’du Center of China Geological Survey, Cheng’du 610081, China
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Junsheng Nie;
Junsheng Nie
4
Key Laboratory of Western China’s Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China
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Yong Xu;
Yong Xu
1
Research Center for Orogenic Geology, Xi’an Center of China Geological Survey, Xi’an 710054, China
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Leping Yue
Leping Yue
2
State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi’an 710069, China
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Feng Pan
1
Research Center for Orogenic Geology, Xi’an Center of China Geological Survey, Xi’an 710054, China2
State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi’an 710069, China
Jianxing Li
3
Cheng’du Center of China Geological Survey, Cheng’du 610081, China
Junsheng Nie
4
Key Laboratory of Western China’s Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China
Yong Xu
1
Research Center for Orogenic Geology, Xi’an Center of China Geological Survey, Xi’an 710054, China
Leping Yue
2
State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi’an 710069, China
Publisher: Geological Society of America
Received:
05 Aug 2021
Revision Received:
02 Jul 2022
Accepted:
19 Oct 2022
First Online:
11 Jan 2023
Online ISSN: 1943-2674
Print ISSN: 0016-7606
© 2023 Geological Society of America
GSA Bulletin (2023)
Article history
Received:
05 Aug 2021
Revision Received:
02 Jul 2022
Accepted:
19 Oct 2022
First Online:
11 Jan 2023
Citation
Feng Pan, Jianxing Li, Junsheng Nie, Yong Xu, Leping Yue; Provenance of eolian deposits in the Xorkol Basin: Implications for Eocene dust-transport pattern in western China. GSA Bulletin 2023; doi: https://doi.org/10.1130/B36274.1
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Index Terms/Descriptors
- absolute age
- Asia
- Cenozoic
- China
- clastic rocks
- claystone
- depositional environment
- Eocene
- Far East
- ICP mass spectra
- laser ablation
- laser methods
- mass spectra
- nesosilicates
- orthosilicates
- paleocirculation
- paleoclimatology
- Paleogene
- paleogeography
- provenance
- sedimentary rocks
- silicates
- spectra
- Tertiary
- U/Pb
- winds
- X-ray fluorescence spectra
- zircon
- zircon group
- western China
- Xorkol Basin
- Xishuigou Formation
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