Provenance and Fluvial‐Aeolian Process of Kyzylkum Desert: Constrained by Detrital Zircon U–Pb Dating

Abstract The Kyzylkum Desert, as a transition area of different dust source in Central Asia, provides and reserves a large amount of dust transported by different atmospheric circulation systems, affecting Uzbekistan and downwind East Asia. However, there remains very few investigations about sedime...

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Main Authors: Mingyu Zhang, Yougui Song, Shukhrat Shukurov, Linghao Zhao, Nosir Shukurov, Xiulan Zong
Format: Article
Language:English
Published: Wiley 2024-07-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2024GL108951
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author Mingyu Zhang
Yougui Song
Shukhrat Shukurov
Linghao Zhao
Nosir Shukurov
Xiulan Zong
author_facet Mingyu Zhang
Yougui Song
Shukhrat Shukurov
Linghao Zhao
Nosir Shukurov
Xiulan Zong
author_sort Mingyu Zhang
collection DOAJ
description Abstract The Kyzylkum Desert, as a transition area of different dust source in Central Asia, provides and reserves a large amount of dust transported by different atmospheric circulation systems, affecting Uzbekistan and downwind East Asia. However, there remains very few investigations about sediment sources and control factors of the desert. We hereby first present a provenance study on the Kyzylkum Desert, utilizing detrital zircon U‐Pb ages of samples composed of desert sand, alluvial sediments from Amu Darya River and piedmont of Southwest Tianshan Mountains. The results reveal that the Southwest Tianshan Mountains contribute the majority of the Kyzylkum desert sand, and the river system, dominated by Syr Darya, controls the sediment provenance of the desert. Moreover, little contribution from the Kyzylkum and Nurata segments indicates that wind erosion on the bedrocks is weak. However, the aeolian process is still crucial but deposit and storage of dust are determined by local topography.
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series Geophysical Research Letters
spelling doaj-art-e4477386f3df4a10bdc8ee2496debbc02025-08-20T02:04:21ZengWileyGeophysical Research Letters0094-82761944-80072024-07-015113n/an/a10.1029/2024GL108951Provenance and Fluvial‐Aeolian Process of Kyzylkum Desert: Constrained by Detrital Zircon U–Pb DatingMingyu Zhang0Yougui Song1Shukhrat Shukurov2Linghao Zhao3Nosir Shukurov4Xiulan Zong5State Key Laboratory of Loess and Quaternary Geology (SKLLQG) Institute of Earth Environment Chinese Academy of Sciences Xi'an PR ChinaState Key Laboratory of Loess and Quaternary Geology (SKLLQG) Institute of Earth Environment Chinese Academy of Sciences Xi'an PR ChinaKh.M. Abdullaev's Institute of Geology and Geophysics University of Geological Sciences Ministry of Mining Industry and Geology of the Republic of Uzbekistan Tashkent UzbekistanKey Laboratory of Deep‐Earth Dynamics Ministry of Natural Resources National Research Center for Geoanalysis Beijing PR ChinaKh.M. Abdullaev's Institute of Geology and Geophysics University of Geological Sciences Ministry of Mining Industry and Geology of the Republic of Uzbekistan Tashkent UzbekistanState Key Laboratory of Loess and Quaternary Geology (SKLLQG) Institute of Earth Environment Chinese Academy of Sciences Xi'an PR ChinaAbstract The Kyzylkum Desert, as a transition area of different dust source in Central Asia, provides and reserves a large amount of dust transported by different atmospheric circulation systems, affecting Uzbekistan and downwind East Asia. However, there remains very few investigations about sediment sources and control factors of the desert. We hereby first present a provenance study on the Kyzylkum Desert, utilizing detrital zircon U‐Pb ages of samples composed of desert sand, alluvial sediments from Amu Darya River and piedmont of Southwest Tianshan Mountains. The results reveal that the Southwest Tianshan Mountains contribute the majority of the Kyzylkum desert sand, and the river system, dominated by Syr Darya, controls the sediment provenance of the desert. Moreover, little contribution from the Kyzylkum and Nurata segments indicates that wind erosion on the bedrocks is weak. However, the aeolian process is still crucial but deposit and storage of dust are determined by local topography.https://doi.org/10.1029/2024GL108951detrital zircon U‐Pb agesriver‐fed desertsfluvial/aeolian processKyzylkum DesertCentral Asia
spellingShingle Mingyu Zhang
Yougui Song
Shukhrat Shukurov
Linghao Zhao
Nosir Shukurov
Xiulan Zong
Provenance and Fluvial‐Aeolian Process of Kyzylkum Desert: Constrained by Detrital Zircon U–Pb Dating
Geophysical Research Letters
detrital zircon U‐Pb ages
river‐fed deserts
fluvial/aeolian process
Kyzylkum Desert
Central Asia
title Provenance and Fluvial‐Aeolian Process of Kyzylkum Desert: Constrained by Detrital Zircon U–Pb Dating
title_full Provenance and Fluvial‐Aeolian Process of Kyzylkum Desert: Constrained by Detrital Zircon U–Pb Dating
title_fullStr Provenance and Fluvial‐Aeolian Process of Kyzylkum Desert: Constrained by Detrital Zircon U–Pb Dating
title_full_unstemmed Provenance and Fluvial‐Aeolian Process of Kyzylkum Desert: Constrained by Detrital Zircon U–Pb Dating
title_short Provenance and Fluvial‐Aeolian Process of Kyzylkum Desert: Constrained by Detrital Zircon U–Pb Dating
title_sort provenance and fluvial aeolian process of kyzylkum desert constrained by detrital zircon u pb dating
topic detrital zircon U‐Pb ages
river‐fed deserts
fluvial/aeolian process
Kyzylkum Desert
Central Asia
url https://doi.org/10.1029/2024GL108951
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