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Open AccessArticle

Indium Mineralization in the Xianghualing Sn-Polymetallic Orefield in Southern Hunan, Southern China

by 1,2, 1,2, 1,2, 1,2,* and 1,2
1
Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring (Central South University), Ministry of Education, Changsha 410083, China
2
School of Geosciences and Info-Physics, Central South University, Changsha 410083, China
*
Author to whom correspondence should be addressed.
Minerals 2017, 7(9), 173; https://doi.org/10.3390/min7090173
Received: 28 July 2017 / Revised: 30 August 2017 / Accepted: 15 September 2017 / Published: 18 September 2017
Although numerous W–Sn–Pb–Zn polymetallic deposits are located in southern Hunan, and In-bearing deposits are related to W–Sn–Pb–Zn polymetallic deposits, Indium mineralization in southern Hunan is poorly studied. In order to investigate the In mineralization of the Xianghualing orefield, which is a typical orefield in southern Hunan, ore bulk chemistry, microscopic observation, and electron-probe microanalysis of vein-type (type-I) and porphyry-type (type-II) Sn–Pb–Zn orebodies were studied. The In contents of the type-I orebodies varies from 0.79 to 1680 ppm (avg. 217 ppm, n = 29), and that of the type-II orebodies varies from 10 to 150 ppm (avg. 64 ppm, n = 10). Although chalcopyrite and stannite contain trace amounts of In, sphalerite is the most important In-rich mineral in the orefield. Sphalerite in type-I orebodies contains from <0.02 to 21.96 wt % In, and in type-II orebodies contains from <0.02 to 0.39 wt % In. Indium-rich chemical-zoned sphalerite contains 7 to 8 wt % In in its core and up to 21.96 wt % In in its rim. This sphalerite may be the highest In-bearing variety in Southern China. The Cd contents of the In-rich sphalerite ranges from 0.35 to 0.45 wt %, which places it in the the “Indium window” of the Cu–In–S phases. The geological and structural features of the Xianghualing orefield indicate that the In mineralization of the two types of In-bearing Sn–Pb–Zn orebodies is related to the volatile-rich, In-rich, A-type granites, and is controlled by the normal faults of magmatic-diapiric activity extensional features. View Full-Text
Keywords: indium; In-bearing sphalerite; Sn-polymetallic deposits; Xianghualing orefield; southern China indium; In-bearing sphalerite; Sn-polymetallic deposits; Xianghualing orefield; southern China
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MDPI and ACS Style

Liu, J.; Rong, Y.; Zhang, S.; Liu, Z.; Chen, W. Indium Mineralization in the Xianghualing Sn-Polymetallic Orefield in Southern Hunan, Southern China. Minerals 2017, 7, 173. https://doi.org/10.3390/min7090173

AMA Style

Liu J, Rong Y, Zhang S, Liu Z, Chen W. Indium Mineralization in the Xianghualing Sn-Polymetallic Orefield in Southern Hunan, Southern China. Minerals. 2017; 7(9):173. https://doi.org/10.3390/min7090173

Chicago/Turabian Style

Liu, Jianping; Rong, Yanan; Zhang, Shugen; Liu, Zhongfa; Chen, Weikang. 2017. "Indium Mineralization in the Xianghualing Sn-Polymetallic Orefield in Southern Hunan, Southern China" Minerals 7, no. 9: 173. https://doi.org/10.3390/min7090173

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