Indium Mineralization in the Yejiwei Sn‐Polymetallic Deposit of the Shizhuyuan Orefield, Southern Hunan, China

• Published in: Resource geology 2018-01, Vol.68 (1), p.22-36
• Main Authors: Liu, Jianping, Rong, Yanan, Gu, Xiangping, Shao, Yongjun, Lai, Jianqing, Chen, Weikang
• Format: Article
• Language: English
• Subjects: Cassiterite; Chalcopyrite; Composition; Copper; Electron microprobe; Exploration; Igneous rocks; Indium; In‐sphalerite; Lead; Marble; Mineralization; Minerals; Molybdenum; Ores; porphyry–skarn–veinlet mineralization; Pyrite; Pyrrhotite; Resources; Silver; Sn‐polymetallic deposit; south Hunan; Sphalerite; Tin; Tungsten; Veins (geology); Yejiwei deposit; Zinc; Zincblende
• ISSN: 1344-1698; 1751-3928
• DOI: 10.1111/rge.12144

The Yejiwei deposit, which is located in the southern Hunan W–Sn–Pb–Zn Metallogenic Belt in south China, is a large‐scale porphyry–skarn–veinlet‐type deposit containing 806 t In. Mineralization occurs as porphyry‐type Sn (stockworks), skarn‐type Sn–Cu, marble‐hosted‐type Sn–Cu (veinlet), and vein‐type Pb–Zn ores. Thirty‐five ore samples were collected from the Yejiwei deposit for bulk and mineral chemical composition, microscopic observation and electron microprobe analyses. The porphyry‐type Sn ores contain variable amounts of In (2.3–76 ppm; mean of 17.4 ppm) with local In enrichment (226 ppm) and 1000 × In/Zn values are 3.8–52.4. The skarn‐type Cu–Sn ore is richest in In (12.3–214 ppm; mean of 114 ppm), and 1000 × In/Zn values are 2.4–117. In contrast, the In content of the marble‐hosted‐type Cu–Sn ores is relatively low (7.4–34.9 ppm; mean of 20.3 ppm), and 1000 × In/Zn is in the range of 0.61–5.5, and the vein‐type Pb–Zn ores in the external zone contain the lowest In contents (7.2–17.0 ppm; mean of 12.1 ppm) with 1000 × In/Zn values of 0.07–0.09. The ore minerals in the deposit include pyrite, pyrrhotite, cassiterite, and In‐bearing minerals of sphalerite, chalcopyrite, and stannite. Although only trace amounts of sphalerite are hosted in the porphyry ores, the sphalerite contains the highest In content (0.27–10.1 wt.% In) in the deposit. We observed the highest In contents of all In‐bearing sphalerite reported in China. The In contents of sphalerite in the skarn‐type ore range from 0.15 to 0.56 wt.%, whereas the marble‐hosted‐, and vein‐type ores have lower In contents (0.00–0.04, and 0.03–0.06 wt.%, respectively). The In resources of the Yejiwei deposit are mainly hosted in skarn ores of the No. 31 and No. 32 orebodies. The genesis of In in the Yejiwei deposit was closely related to the shallow intrusive environment of related igneous rocks. As W–Sn–Mo–Bi–Cu–Pb–Zn–Ag mineralization is widespread in south Hunan, this study would suggest a focus on skarn‐type Sn–Zn deposits for the future prospecting of In resources. The Yejiwei is a porphyry–skarn–veinlet‐type Sn‐polymetallic deposit containing 806 t of In. Ore geochemical data shows skarn‐type ore is relatively enriched in In (12.25–214 ppm; mean of 114.43 ppm). In contrast, porphyry Sn ores, veinlets ores, and Pb–Zn‐rich veins contains lower In. The In‐rich sphalerite containing 8.7–10.1 wt.% In was found, which represents the most In‐riched sphalerite reported in China.