Geology, mineralization, fluid inclusion, and stable isotope characteristics of the Zaghar and Sarabadan Cu-(Au) skarn deposits, Tafresh, Central Iran

The Zaghar and Sarabadan copper-(gold) deposits are located in the northern part of the Urumieh-Dokhtar magmatic belt. Mineralization occurred in contact of the post-Eocene diorite-tonalite stocks with the upper Triassic-Jurassic shale and sandstone series in the Zaghar, and lower Eocene volcanic and pyroclastic rocks in the Sarabadan. Based on field observation and mineralogical studies, three stages of mineralization can be distinguished: (1) prograde skarn; (2) retrograde skarn; and (3) supergene stages. The prograde skarn is characterized by association of andradite, diopside, cordierite, and minor actinolite. The retrograde skarn stage is divided into two sub-stages: (1) retrograde skarn I; and retrograde skarn II. The retrograde skarn I, is marked by deposition of the main alteration minerals (e.g., tremolite, actinolite, chlorite, epidote), magnetite, ilmenite, pyrrhotite, pyrite, barite, and small amount of other sulfide minerals. The retrograde skarn II or quartz-sulfide-carbonate stage, is characterized by quartz and calcite vein-veinlets associated with Cu-Au mineralization. The supergene stage is marked by Fe oxy-hydroxides, covellite, malachite, azurite, and minor clay minerals and calcite. Ore-forming fluids associated with the quartz, calcite, and sphalerite from the retrograde II stage of mineralization is represented by LVS fluid inclusions with the temperature of 218-512 degrees C and salinity of 6.73-59.09 wt% NaCl, and LV type fluids with the temperature of 130-215 degrees C and salinity of 1.70-30.00 wt% NaCl equivalent. Stable isotope analysis of quartz yielded values of -85.30 to -60.70 delta D parts per thousand, and +7.82-9.60 parts per thousand delta O-18(fluid), indicating that the ore-forming fluids were mainly magmatic fluids with some contributions from meteoric waters. The delta S-34 values of pyrite vary from +4.90-8.10 parts per thousand, demonstrate that the sulfur in deposit was probably originated from the magma. The geological and geochemical features introduce the Zaghar and Sarabadan as Cu-(Au) skarn deposits are related to the magmatic-hydrothermal activity of diorite stocks within continental magmatic arc.