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Minerals 2016, 6(2), 42; doi:10.3390/min6020042

Sn-Bearing Minerals and Associated Sphalerite from Lead-Zinc Deposits, Kosovo: An Electron Microprobe and LA-ICP-MS Study

Department of Economic Geology, Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, al. Mickiewicza 30, Kraków 30-059, Poland
Department of Mineralogy and Petrology, Faculty of Geology & Geoenvironment, National and Kapodistrian University of Athens, Athens 15784, Greece
Department of Mineralogy, Petrology and Economic Geology, Faculty of Geology, Aristotle University of Thessaloniki, Thessaloniki 54124, Greece
E & E Experts LLC, Prishtina 10000, Republic of Kosovo
Author to whom correspondence should be addressed.
Academic Editor: Federica Zaccarini
Received: 9 March 2016 / Revised: 26 April 2016 / Accepted: 28 April 2016 / Published: 6 May 2016
(This article belongs to the Special Issue Advanced Research on Accessory Minerals)
View Full-Text   |   Download PDF [3582 KB, uploaded 6 May 2016]   |  


Stannite group minerals (ferrokësterite and stannite) occur in small amounts in association with sulfides in hydrothermal Pb-Zn deposits in Kosovo. The chemical composition of sphalerite co-existing with Sn-bearing minerals has been investigated using laser ablation inductively-coupled plasma mass spectrometry (LA-ICP-MS). Flat Sn-spectra suggest that Sn is bound in the sphalerite lattice or as nanoincluions. Sphalerite from Stan Terg, overgrown by ferrokësterite, contains the lowest Sn content (few ppm) and have been precipitated before Sn-enrichment in the fluids. The highest value of Sn (520 ppm) of Stan Terg sphalerite was obtained directly close to the ferrokësterite rim, and indicates a rapid increase of Sn in the hydrothermal fluids. Significantly higher values of Sn in sphalerite were obtained from other deposits: 1600 ppm (Artana), up to 663 ppm (Kizhnica), up to 2800 ppm (Drazhnje). Stannite-sphalerite geothermometry revealed the following ore-forming temperatures for the Kosovo mineralization: 240–390 °C for Stan Terg, 240–370 °C for Artana, >340 °C for Kizhnica, and 245–295 °C for Drazhnje. Sphalerite and stannite group minerals precipitated simultaneously during cooling from reduced hydrothermal fluids and under low-sulfidation fluid states. Fluctuations in physico-chemical fluid conditions are evidenced by the presence of stannite group minerals along growth zones in sphalerite and may be related to short interval of magmatic pulses during ore deposition. View Full-Text
Keywords: stannite group minerals; sphalerite; LA-ICP-MS study; Trepça Mineral Belt; Kosovo stannite group minerals; sphalerite; LA-ICP-MS study; Trepça Mineral Belt; Kosovo

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MDPI and ACS Style

Kołodziejczyk, J.; Pršek, J.; Voudouris, P.; Melfos, V.; Asllani, B. Sn-Bearing Minerals and Associated Sphalerite from Lead-Zinc Deposits, Kosovo: An Electron Microprobe and LA-ICP-MS Study. Minerals 2016, 6, 42.

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