engleski

Mineralogical, fluid inclusion and stable isotope characteristics of the Sasa Pb-Zn skarn deposit, Republic of Macedonia

In the Sasa Pb-Zn deposit the mineralization is represented by skarn and hydrothermal mineral parageneses that are hosted by the medium to coarse grained cipollino marble of the late Paleozoic age. The skarn parageneses comprise anhydrous Ca-Fe- -Mn silicate minerals, such as pyroxenes and pyroxenoids (a prograde skarn assemblage), and hydrous silicates, including epidote and chlorites, accompanied with magnetite, carbonates and quartz (a retrograde skarn assemblage). The hydrothermal parageneses are characterized by the presence of galena, sphalerite, pyrite and chalcopyrite. Carbonates and quartz are the most abundant hydrothermal gangue minerals.

skarn deposit; fluid inclusions; stable isotopes; mineralogy

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