Occurrence of cobalt and its geological significance in the Qibaoshan Co-Pb-Zn deposit, central segment of the Jiangnan orogenic belt

KUANG Erlong; CHEN Zhikang; ZHOU Jiangtao; LI Guomeng; JIANG Baoliang; LUO Xicheng; LI Yanjun

doi:10.19509/j.cnki.dzkq.tb20240410

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KUANG Erlong，CHEN Zhikang，ZHOU Jiangtao，et al. Occurrence of cobalt and its geological significance in the Qibaoshan Co-Pb-Zn deposit, central segment of the Jiangnan orogenic belt[J]. Bulletin of Geological Science and Technology，2025，44（6）：1-16 doi: 10.19509/j.cnki.dzkq.tb20240410

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Occurrence of cobalt and its geological significance in the Qibaoshan Co-Pb-Zn deposit, central segment of the Jiangnan orogenic belt

doi: 10.19509/j.cnki.dzkq.tb20240410

KUANG Erlong^{1, 2
,},
CHEN Zhikang³,
ZHOU Jiangtao³,
LI Guomeng^{1, 2},
JIANG Baoliang^{1, 2},
LUO Xicheng^{1, 2},
LI Yanjun^{3
,
,}

1 .
The First Geological Brigade, Jiangxi Bureau of Geology, Nanchang 330052, China
2 .
Jiangxi Exploration Breakthrough Technology Center, Nanchang 330052, China
3 .
School of Earth Resources, China University of Geosciences (Wuhan), Wuhan 430074, China

More Information

Author Bio:
E-mail：526167758@qq.com
Corresponding author: E-mail: liyj@cug.edu.cn
Received Date: 23 Jul 2024
Accepted Date: 06 Nov 2024
Rev Recd Date: 27 Oct 2024

Available Online: 28 Oct 2025

Abstract

Abstract

Objective
Cobalt is an important strategic metal, crucial for new energy technologies. Understanding its occurrence in ore deposits represents a key focus of international ore deposit research. The Qibaoshan Co-Pb-Zn deposit, located in the central segment of the Jiangnan orogenic belt, features ore bodies controlled by secondary folds within the core of the Gaodongshan anticline, which exhibit NE-trending lenticular or stratoid shapes. However, the occurrence state of cobalt in this deposit remains poorly constrained.
Methods
In this study, ore samples collected from different levels of the open pit were analyzed using backscattered electronc (BSE) imaging, energy dispersive X-ray spectroscopy (EDS), and electron probe micro analysis (EPMA).
Results
The results show that cobalt occurs predominantly as independent minerals, including safflorite, cobaltite, skutterudite, and siegenite. Minor cobalt is hosted in solid solution within fine-grained pyrite and rammelsbergite. Rammelsbergite commonly exhibits mantles replaced by safflorite, and both minerals are in turn replaced at their rims by cobaltite and gersdorffite. Cobaltite and Cu-bearing siegenite also frequently replace the margins of chalcopyrite. These mineralogical relationships indicate that the early-stage ore-forming fluids were characterized by high arsenic activity, leading to the precipitation of rammelsbergite, safflorite, and skutterudite. As mineralization proceeded, arsenic activity decreased while sulfur activity increased, resulting in the formation of cobaltite and siegenite during the late stage.
Conclusions
The replacement textures and mineral assemblages of Co-Ni minerals in the Qibaoshan deposit resemble those typical of "five-element vein"-type deposits. Therefore, the Qibaoshan deposit is classified as a hydrothermal vein-type Co-Pb-Zn deposit with characteristics of "five-element vein".
- cobalt deposit,
- occurrence mod,
- hydrothermal vein type,
- Qibaoshan,
- central segment of the Jiangnan orogenic belt

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References(75)

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Occurrence of cobalt and its geological significance in the Qibaoshan Co-Pb-Zn deposit, central segment of the Jiangnan orogenic belt

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Occurrence of cobalt and its geological significance in the Qibaoshan Co-Pb-Zn deposit, central segment of the Jiangnan orogenic belt

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