广西东平锰矿床地质地球化学特征及矿床成因

周皓宇; 皮道会; 黄钦; 丁大庆; 凌泽

doi:10.3799/dqkx.2022.159

Volume 49 Issue 2

Feb. 2024

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Zhou Haoyu, Pi Daohui, Huang Qin, Ding Daqing, Ling Ze, 2024. Geology, Geochemistry and Genesis of the Dongping Manganese Deposit, Guangxi Province, China. Earth Science, 49(2): 656-668. doi: 10.3799/dqkx.2022.159

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Zhou Haoyu, Pi Daohui, Huang Qin, Ding Daqing, Ling Ze, 2024. Geology, Geochemistry and Genesis of the Dongping Manganese Deposit, Guangxi Province, China. Earth Science, 49(2): 656-668. doi: 10.3799/dqkx.2022.159

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Geology, Geochemistry and Genesis of the Dongping Manganese Deposit, Guangxi Province, China

doi: 10.3799/dqkx.2022.159

Zhou Haoyu^{1, 2
,
,},
Pi Daohui^{2
,
,
,},
Huang Qin²,
Ding Daqing^{3, 4},
Ling Ze⁵

1.
No.313 Geological Party of Anhui Bureau of Geology and Mineral Exploration, , Lu'an 237010, China
2.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
3.
China Metallurgical Geology Bureau of Geological Prospecting Institute of Guangxi, Nanning 530022, China
4.
Institute of Mineral Resources Research, China Metallurgical Geology Bureau, Beijing 101300, China
5.
Liaoning Fourth Geological Team Limited Liability Company, Fuxin 123000, China

Received Date: 2022-12-28
Publish Date: 2024-02-25

Abstract

Abstract

Triassic is one of the most important manganese (Mn) metallogenic epoch, and there are many great to medium sized Mn ore deposits in South China. Dongping manganese deposit is located in the metallogenic belt of southwest Guangxi Zhuang Autonomous Region. In this paper, we discussed sources and genesis of Mn ore deposit by detailed petrographic observations using optical microscope and electron probe micro analysis (EPMA) and geochemical analysis. Based on detailed petrographic observations, we found various metal sulfides, inculding pyrite, chalcopyrite, sphalerite, galena, siegenite, cobalite and other sulfoarsenide in Dongping Mn ore deposit. The Al/(Al+Fe+Mn) and Y/Ho ratio, Fe-Mn-(Ni+Cu+Co)×10 and lgU-lgTh graphs of Mn ores indicated that source of Mn is associated with hydrothermal activity. The positive Ce anomaly and V/(V+Ni) of Mn ores indicate that Mn was initially precipitated in oxic environment. Combining all data, we suggest that source of Mn is associated with hydrothermal activity. Manganese carbonate formed by reduction of Mn oxides derived from hydrothermal activity during the diagenesis.
- Dongping manganese deposit,
- geochemistry,
- source of ore-forming material,
- metallogenesis model

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Geology, Geochemistry and Genesis of the Dongping Manganese Deposit, Guangxi Province, China

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