Genesis of the newly discovered Pb–Zn vein of the Sucha giant fluorite deposit in Inner Mongolia: Constraints from LA-ICP-MS trace element of pyrite and sphalerite

Jiang, Biao; Wang, Denghong; Pu, Xiulang; Liu, Yu; Chen, Yuchuan; Wang, Wenjun; Ma, Wenwen; Wang, Chengliang; Wang, Qiang; Chen, Wei

doi:10.1016/j.apgeochem.2023.105801

Applied Geochemistry

2023

DOI: 10.1016/j.apgeochem.2023.105801

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Genesis of the newly discovered Pb–Zn vein of the Sucha giant fluorite deposit in Inner Mongolia: Constraints from LA-ICP-MS trace element of pyrite and sphalerite

Biao Jiang,

Denghong Wang,

Xiulang Pu

et al.

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2024

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Cited by 2 publications

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Genesis of Yongping copper deposit in the Qin-Hang Metallogenic Belt, SE China: Insights from sulfide geochemistry and sulfur isotopic data

Shi,

Fan,

et al. 2024

Ore Geology Reviews

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Genesis of Yongping copper deposit in the Qin-Hang Metallogenic Belt, SE China: Insights from sulfide geochemistry and sulfur isotopic data

Shi,

Fan,

et al. 2024

Ore Geology Reviews

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Study of Enrichment and Conversion Mechanisms of Heavy Metal Elements in Mines in Cold Regions Under Freezing and Thawing

Zhang,

Zhu,

Zhang

et al. 2024

Water

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In cold-region mines, the dual effects of heat islands and cold islands, caused by cycling of hot and cold temperature extremes, facilitate the outward dispersion of heavy metal dust. Freeze–thaw cycles occurring in ice provide a conducive environment for the enrichment and conversion of heavy metals, allowing them to enter downstream rivers with meltwater. This process significantly impacts human activities and ecosystems in areas traversed by these rivers. This study is conducted in the typical alpine mining area in Xinjiang, China, and focuses on the impact of freeze–thaw cycles on the enrichment and conversion of heavy metals in alpine mining regions. It employs a comprehensive approach combining field measurements, environmental simulations, theoretical analysis, and laboratory experiments. The findings indicate that the environmental behavior of heavy metals is influenced not only by the freeze–thaw cycles themselves but also by factors such as temperature, pH, and redox conditions. Heavy metal elements may enter water bodies during the melting process and pose risks to downstream ecosystems and human health.

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Genesis of the newly discovered Pb–Zn vein of the Sucha giant fluorite deposit in Inner Mongolia: Constraints from LA-ICP-MS trace element of pyrite and sphalerite

Cited by 2 publications

References 52 publications

Genesis of Yongping copper deposit in the Qin-Hang Metallogenic Belt, SE China: Insights from sulfide geochemistry and sulfur isotopic data

Genesis of Yongping copper deposit in the Qin-Hang Metallogenic Belt, SE China: Insights from sulfide geochemistry and sulfur isotopic data

Study of Enrichment and Conversion Mechanisms of Heavy Metal Elements in Mines in Cold Regions Under Freezing and Thawing

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