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Minerals, Volume 15, Issue 9
September 2025 - 118 articles
Cover Story: Gold mineralization at Ity (Ivory Coast) is associated with skarns at contacts between Birimian volcano–sedimentary rocks and felsic intrusions, whereas at nearby Dahapleu, it is structurally controlled in shear zones. Fluid inclusions reveal a hybrid model: a mesothermal orogenic system dominated by CO2–CH4 fluids at >350 °C, superimposed on skarn-related mineralization. A late Bi–Te–Au–Ag stage at ~200–300 °C reflects hydrothermal overprint. At Dahapleu, volatile-rich inclusions (CO2, CO2–CH4, CO2–N2) indicate metamorphic fluids circulating in convective fault systems, with distinct fluid–rock interactions. Overall, these two mineralisations record a long-lived thermal anomaly combining skarn formation, shear deformation, and hydrothermal activity. View this paper
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Minerals - ISSN 2075-163X