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

Autori
Šmajgl, Danijela ; Strmić Palinkaš, Sabina ; Palinkaš, Ladislav ; Spangenberg, Jorge, E. ; Čobić, Andrea ; Bermanec, Vladimir ; Tasev, Goran ; Serafimovski, Todor ; Peltekovski Zlatko

Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni

Izvornik
Buletini I Shkencave Gjeologjike 2/2014, Proceedings XX congress of the Carpathian- Balkan Geological Association / Ionescu C. ; Christofides G. ; Uta A. ; Beqiraj Goga E. ; Marku S. - Tirana, 2014, 233-233

Skup
XX congress of the Carpathian- Balkan Geological Association

Mjesto i datum
Tirana, Albanija, 24.09.2014. - 26.09.2014

Vrsta sudjelovanja
Predavanje

Vrsta recenzije
Međunarodna recenzija

Ključne riječi
skarn deposit; fluid inclusions; stable isotopes; mineralogy

Sažetak
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.

Izvorni jezik
Engleski

Znanstvena područja
Geologija

POVEZANOST RADA