Automated Mineralogy for Gold Deportment: A Case Study of a Skarn Fe–Au–Polymetallic Deposit in the Eastern Kunlun Orogenic Belt, NW China

Gold deportment data are essential for understanding mineralization mechanisms and guiding beneficiation and metal recovery. Scanning electron microscope (SEM)-based automated mineralogy (SEM-AM) allows for the numeric assessment of ores’ compositional and textural properties. In this study, a new SEM-AM technique, BGRIMM Process Mineralogy Analyzing System, abbreviated as BPMA, was employed to characterize the gold deportment of a skarn Fe–Au–polymetallic deposit in the Eastern Kunlun Orogenic Belt (EKOB), NW China. The results show that the gold minerals in the ore are primarily native gold (Au), which contributes 78.27% of the Au, followed by maldonite (Au2Bi), which contributes 21.73% of the Au; the iron minerals consist mainly of magnetite, with a mass fraction of 23.00 wt%, contributing approximately 63.37% of the iron. The native gold is mainly intimately associated with grossular and magnetite, while the maldonite mainly coexists with arsenopyrite–(Co), löllingite–(Co), bismuth, and tetradymite, forming a complex and unique Au–Bi–(Te)–As–S±Co mineral/element group and texture. This indicates that the liquid bismuth collector mechanism could be a plausible hypothesis for enrichment, migration, and precipitation during mineralization, consistent with the observed textures. The nuggets primarily exist in the form of intergranular gold (37.04 wt%) and fissure gold (35.13 wt%), followed by inclusion gold (26.30 wt%). The grain size of nuggets is very fine; 94.32 wt% of gold grains are less than 10 μm. The grain sizes of the main gold-carrying minerals [i.e., magnetite and arsenopyrite–(Co)] are mainly distributed in coarse-grained size fractions (>295 μm) and medium-grained size fractions (+74 μm, −295 μm), making them easy to liberate during grinding. A preliminary recommendation of a principle flowsheet of “flotation for gold recovery–magnetic separation of flotation tailings for iron recovery–flotation desulfurization of magnetic concentrate” at a grind size of 65% passing 74 μm was proposed for gold and iron recovery.

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Journal
Minerals
Published
2026-10-13
DOI
https://doi.org/10.3390/min16101042
Primary Topic
Geochemistry and Geochronology of Asian Mineral Deposits
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article
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article

Automated Mineralogy for Gold Deportment: A Case Study of a Skarn Fe–Au–Polymetallic Deposit in the Eastern Kunlun Orogenic Belt, NW China

Jia Mu-xin, 温利刚, Jianjun Zhao, Qing Wang et al.
Minerals
Geochemistry and Geochronology of Asian Mineral Deposits
article

Automated Mineralogy for Gold Deportment: A Case Study of a Skarn Fe–Au–Polymetallic Deposit in the Eastern Kunlun Orogenic Belt, NW China

Jia Mu-xin, 温利刚, Jianjun Zhao, Qing Wang, Hongyu Lu, Zhu Yang-ge, Zhi-Kai Hu, Yun Fu, Lei Zhang, Chao Huang
article en

Abstract

Gold deportment data are essential for understanding mineralization mechanisms and guiding beneficiation and metal recovery. Scanning electron microscope (SEM)-based automated mineralogy (SEM-AM) allows for the numeric assessment of ores’ compositional and textural properties. In this study, a new SEM-AM technique, BGRIMM Process Mineralogy Analyzing System, abbreviated as BPMA, was employed to characterize the gold deportment of a skarn Fe–Au–polymetallic deposit in the Eastern Kunlun Orogenic Belt (EKOB), NW China. The results show that the gold minerals in the ore are primarily native gold (Au), which contributes 78.27% of the Au, followed by maldonite (Au2Bi), which contributes 21.73% of the Au; the iron minerals consist mainly of magnetite, with a mass fraction of 23.00 wt%, contributing approximately 63.37% of the iron. The native gold is mainly intimately associated with grossular and magnetite, while the maldonite mainly coexists with arsenopyrite–(Co), löllingite–(Co), bismuth, and tetradymite, forming a complex and unique Au–Bi–(Te)–As–S±Co mineral/element group and texture. This indicates that the liquid bismuth collector mechanism could be a plausible hypothesis for enrichment, migration, and precipitation during mineralization, consistent with the observed textures. The nuggets primarily exist in the form of intergranular gold (37.04 wt%) and fissure gold (35.13 wt%), followed by inclusion gold (26.30 wt%). The grain size of nuggets is very fine; 94.32 wt% of gold grains are less than 10 μm. The grain sizes of the main gold-carrying minerals [i.e., magnetite and arsenopyrite–(Co)] are mainly distributed in coarse-grained size fractions (>295 μm) and medium-grained size fractions (+74 μm, −295 μm), making them easy to liberate during grinding. A preliminary recommendation of a principle flowsheet of “flotation for gold recovery–magnetic separation of flotation tailings for iron recovery–flotation desulfurization of magnetic concentrate” at a grind size of 65% passing 74 μm was proposed for gold and iron recovery.

MineralsVol. 16(10)
Beijing General Research Institute of Mining and Metallurgy (CN), State Key Laboratory of Mineral Processing, Northeastern University (CN)
Openalex Percentile: Top 8%
Geochemistry and Geochronology of Asian Mineral Deposits
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