巴丹吉林沙漠南缘冲洪积物的光释光年代及其水文学意义

姜高磊; 聂振龙; 刘哲; 王哲; 赵华; 杨劲松; 申建梅

doi:10.3799/dqkx.2020.148

Volume 46 Issue 5

May 2021

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Article Navigation > Earth Science > 2021 > 46(5): 1829-1839

Jiang Gaolei, Nie Zhenlong, Liu Zhe, Wang Zhe, Zhao Hua, Yang Jinsong, Shen Jianmei, 2021. OSL Ages and Its Hydrological Implications of Alluvial-Diluvial Deposits from the Southern Margin of Badain Jaran Desert. Earth Science, 46(5): 1829-1839. doi: 10.3799/dqkx.2020.148

Citation:

Jiang Gaolei, Nie Zhenlong, Liu Zhe, Wang Zhe, Zhao Hua, Yang Jinsong, Shen Jianmei, 2021. OSL Ages and Its Hydrological Implications of Alluvial-Diluvial Deposits from the Southern Margin of Badain Jaran Desert. Earth Science, 46(5): 1829-1839. doi: 10.3799/dqkx.2020.148

Citation:

Jiang Gaolei, Nie Zhenlong, Liu Zhe, Wang Zhe, Zhao Hua, Yang Jinsong, Shen Jianmei, 2021. OSL Ages and Its Hydrological Implications of Alluvial-Diluvial Deposits from the Southern Margin of Badain Jaran Desert. Earth Science, 46(5): 1829-1839. doi: 10.3799/dqkx.2020.148

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OSL Ages and Its Hydrological Implications of Alluvial-Diluvial Deposits from the Southern Margin of Badain Jaran Desert

doi: 10.3799/dqkx.2020.148

Jiang Gaolei^{1, 2
,
,},
Nie Zhenlong¹,
Liu Zhe^{1, 2},
Wang Zhe¹,
Zhao Hua^{1, 2},
Yang Jinsong^{1, 2},
Shen Jianmei^{1
,
,
,}

1.
Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China
2.
Key Laboratory of Quaternary Chronology and Hydro-Environment Evolution, China Geological Survey, Shijiazhuang 050061, China

Received Date: 2020-06-08
Publish Date: 2021-05-15

Abstract

Abstract

Alluvial-diluvial deposits can record climatic and hydrologic information in geological history and play an important role in the reconstruction of paleoenvironment. Aqueous deposits were discovered at the south margin of Badain Jaran desert, Northwest China. Based on sedimentological analyses, two sections of the deposits as palaeoflood deposit and paleofluvial deposit were identified. OSL dating suggests that the deposits formed in the Middle Holocene. The alluvial-diluvial deposits in the southern margin of Badain Jaran Desert were mainly formed under a humid climate during the Middle Holocene. Based on the previous paleoclimate study, comprehensive analysis of the location and sedimentary features and the previous research of paleoclimate in this region, a conceptual model of recharge to the Badain Jaran is proposed. During humid climatic phases, such as the Middle Holocene, the precipitation in this region and adjacent mountain areas recharged the groundwater of the desert area by temporary flood or/and intermittent stream.
- Badain Jaran desert,
- alluvial-diluvial deposit,
- OSL dating ages,
- Middle Holocene,
- groundwater recharge,
- hydrogeology

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References(52)

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OSL Ages and Its Hydrological Implications of Alluvial-Diluvial Deposits from the Southern Margin of Badain Jaran Desert

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