新疆库米什盆地硝酸盐类矿床成矿离子迁移规律及成矿模型

李长忠; 程怀德; 宋建国; 马学海; 海擎宇; 蒋天明

doi:10.3799/dqkx.2021.142

Volume 47 Issue 1

Jan. 2022

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Li Changzhong, Cheng Huaide, Song Jianguo, Ma Xuehai, Hai Qingyu, Jiang Tianming, 2022. Ore-Forming Ion Migration Regularity and Metallogenic Model of Nitrate Deposits in Kumishi Basin, Xinjiang. Earth Science, 47(1): 82-93. doi: 10.3799/dqkx.2021.142

Citation:

Li Changzhong, Cheng Huaide, Song Jianguo, Ma Xuehai, Hai Qingyu, Jiang Tianming, 2022. Ore-Forming Ion Migration Regularity and Metallogenic Model of Nitrate Deposits in Kumishi Basin, Xinjiang. Earth Science, 47(1): 82-93. doi: 10.3799/dqkx.2021.142

Citation:

Li Changzhong, Cheng Huaide, Song Jianguo, Ma Xuehai, Hai Qingyu, Jiang Tianming, 2022. Ore-Forming Ion Migration Regularity and Metallogenic Model of Nitrate Deposits in Kumishi Basin, Xinjiang. Earth Science, 47(1): 82-93. doi: 10.3799/dqkx.2021.142

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Ore-Forming Ion Migration Regularity and Metallogenic Model of Nitrate Deposits in Kumishi Basin, Xinjiang

doi: 10.3799/dqkx.2021.142

Li Changzhong^{1, 2, 3
,
,},
Cheng Huaide^{1, 2
,
,
,},
Song Jianguo^{1, 2, 3},
Ma Xuehai^{1, 2, 3},
Hai Qingyu^{1, 2},
Jiang Tianming^{1, 2, 3}

1.
Key Lab of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China
2.
Qinghai Provincial Key Laboratory of Geology and Environment of Salt Lakes, Xining 810008, China
3.
University of Chinese Academy of Sciences, Beijing 100049, China

Received Date: 2021-01-25
Publish Date: 2022-01-20

Abstract

Abstract

In order to understand the spatial distribution characteristics of ore-forming ions and the reason for high nitrate content in surface sediments of nitrate deposits in Kumishi Basin. In this study it focuses on the nitrate deposits in the basin, and a quantitative analysis of the chemical composition of soluble salts in various make-up water samples and soil samples was carried out in the study area. Combined with field geological exploration work, the migration regularity of ore-forming ions in nitrate deposits is discussed. Besides, a model of sedimentary mineralization of nitrate deposits in the basin was established. The results show that ore-forming ions such as K⁺, Na⁺, and NO₃^- migrate and enrich from northwest and southeast toward the middle of the basin. The concentrations of K⁺, Na⁺, NO₃^- and other ore-forming ions gradually increase along the direction of the bedrock area-fan root-middle fan-fan margin in the diluvial fan in the northeast of the basin, and enrichment occurs in the surface sediments at the fan margin. In the vertical profiles, K⁺, Na⁺, NO₃^- and other ore-forming ions mainly show migration and enrichment in the depth range of 0-60 cm. Under the influence of capillarity, they migrated and enriched from deep to surface sediments.
- Kumishi Basin,
- nitrate deposit,
- ore-forming ion,
- sedimentary mineralization model,
- capillary action,
- mineral deposit

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References(59)

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Ore-Forming Ion Migration Regularity and Metallogenic Model of Nitrate Deposits in Kumishi Basin, Xinjiang

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