THE PALEA KAVALA REDUCED INTRUSION-RELATED BI-TE-PB-SB±AU SYSTEM, NORTHEASTERN GREECE: MINERALOGICAL, FLUID INCLUSION, AND SULFUR ISOTOPE STUDIES
The Kavala vein system is comprised of quartz with lesser amounts of K-feldspar, plagioclase and muscovite. Quartz-sericite-pyrite alteration is pervasive but minor kaolinite is also present. Pyrite (~5% of vein volume) contains inclusions of tetradymite (some gold-bearing), bismuthinite, and cosalite. Sulfur isotope values (n = 27) of pyrite from the Kavala and Chalkero veins, as well as pyrite and galena from the Garizo Hill Fe-Mn-Pb vein range from -4.7 to 1‰ and suggest a magmatic sulfur source. Homogenization temperatures (Th) of type I (two-phase aqueous liquid-vapor) and type II (three-phase, H2O-CO2-rich) fluid inclusions that homogenize into the liquid phase in quartz from the Kavala and Chalkero veins range from 216.0º to 420.0ºC (n = 216) and 255.7 º to 414.0 ºC (n = 112), respectively. The Th of type III (two-phase aqueous liquid-vapor), which homogenize into the vapor phase, range from 210.4o to 323.4oC (n = 28). The salinities of type I and type II inclusions range from 15.9 to 22.6 wt. % NaCl equiv. and 5.5 to 11.2 wt. % NaCl equiv., respectively. Eutectic temperatures of -58.5o to -44.3oC for type I inclusions suggest the presence of appreciable CaCl2 in addition to NaCl. The occurrence of a zoned metallogenetic district centered on Bi-Te-Pb-Sb±Au mineralization within the Kavala pluton, and the two high-temperature, high-salinity, immiscible carbonic and aqueous fluids associated with the Kavala and Chalkero veins are consistent with them being part of an RIRGS.