山西省袁家村铁矿成矿时代及成矿环境

李家掀; 胡天杨; 刘磊

doi:10.3799/dqkx.2022.293

Volume 48 Issue 12

Dec. 2023

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Li Jiaxian, Hu Tianyang, Liu Lei, 2023. Metallogenic Age and Metallogenic Environment of Yuanjiacun Iron Deposit in Shanxi Province. Earth Science, 48(12): 4404-4426. doi: 10.3799/dqkx.2022.293

Citation:

Li Jiaxian, Hu Tianyang, Liu Lei, 2023. Metallogenic Age and Metallogenic Environment of Yuanjiacun Iron Deposit in Shanxi Province. Earth Science, 48(12): 4404-4426. doi: 10.3799/dqkx.2022.293

Li Jiaxian, Hu Tianyang, Liu Lei, 2023. Metallogenic Age and Metallogenic Environment of Yuanjiacun Iron Deposit in Shanxi Province. Earth Science, 48(12): 4404-4426. doi: 10.3799/dqkx.2022.293

Citation:

Li Jiaxian, Hu Tianyang, Liu Lei, 2023. Metallogenic Age and Metallogenic Environment of Yuanjiacun Iron Deposit in Shanxi Province. Earth Science, 48(12): 4404-4426. doi: 10.3799/dqkx.2022.293

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Metallogenic Age and Metallogenic Environment of Yuanjiacun Iron Deposit in Shanxi Province

doi: 10.3799/dqkx.2022.293

Li Jiaxian^{1, 2
,
,},
Hu Tianyang^{1, 2},
Liu Lei^{1, 2
,
,}

1.
Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha, 410083, China
2.
School of Geosciences and Info-Physics, Central South University, Changsha 410083, China

Received Date: 2022-03-07
Available Online: 2024-01-03
Publish Date: 2023-12-25

Abstract

Abstract

In order to restrict the age and mineralization of the Yuanjiacun iron deposit and reveal its implications for the paleomarine environment, it determined the detrital zircon U-Pb chronology, major and trace elements of whole rock and trace elements of hematite for BIFs samples which collected from the Yuanjiacun iron deposit. Its detrital zircon U-Pb age constrains the sedimentary age of Yuanjiacun iron ore between 2 200 and 2 235 Ma. The characteristics of major and trace elements indicate that it is a relatively pure sediment and formed by the mixing of seawater and high temperature hydrothermal fluid. And the river input may be one of iron sources during the deposition process. Yuanjiacun iron deposit was formed at the end of the GOE. There are obvious grouping of REE distribution pattern characteristics in Yuanjiacun iron deposit, as well as negative Ce anomaly and slight positive Ce anomaly. This agrees with a reductive and oxidative environment, indicating that the paleomarine environment at that time was characterized by redox stratification. These features suggest a dramatic change in the paleo-marine environment after the GOE, with some degree of oxidation occurring in seawater and shifting from the original single reducing environment to a redox stratified state.
- great oxidation event,
- paleomarine environment evolution,
- Yuanjiacun BIFs,
- hematite trace elements,
- detrital zircon,
- mineral deposit

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References(66)

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