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Minerals, Volume 14, Issue 1
January 2024 - 117 articles
Cover Story: The Sn-W deposits in Krupka ore district are associated with greisens occurring in the upper parts of Late Variscan granitoid intrusions. Fluid inclusions were studied in minerals from greisenized granites, greisens, and hydrothermal veins. The greisenization process took place at temperatures of 370–490 °C and pressures of 155–371 bars, and associated fluids had predominantly low salinity and a low gas content. The post-greisenization stage was connected with the formation of (i) low-salinity (<8 wt. % NaCl eq.) fluid inclusions with homogenization temperatures of <120–295 °C and (ii) high-salinity (>35 wt. % NaCl eq.) fluid inclusions with homogenization temperatures of 140–370 °C, often containing solids. The source of fluids was not only magmatogenic but also in meteoric water or sedimentary rocks. View this paper
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Minerals - ISSN 2075-163X