In the southeastern part of the Cenozoic Urumieh-Dokhtar Magmatic Belt of Iran the NW-trending Kerman Porphyry Copper Belt hosts major porphyry Cu-(Mo-Au) deposits (PCD) of Miocene age; e.g. the diorite-type Cu-Au Meiduk and granodiorite-type Cu-Mo Sar Cheshmeh deposits. The polymetallic vein type deposit Chah-Mesi is located ~ 1.5 km south of the Meiduk porphyry stock. Its genetic relation to the porphyry system is unclear. At Chah-Mesi, Paleocene to Eocene calc-alkaline volcanic and pyroclastic rocks of mainly basaltic-andesitic composition were intruded by Miocene microdioritic dykes. The host rocks were affected by intense hydrothermal alteration exhibiting a central zone of strong silicification that grades into sericitization and propylitic alteration towards the peripheral parts. Argillic alteration is restricted to superficial areas and in direction to the Meiduk PCD propylitic alteration changes into potassic alteration. Six different vein types are distinguished: including two porphyry-related vein types, three alteration-related types of veinlets as well as mineralized veins showing massive, banded, crustiform and brecciated textures. Mineralization occurs as open space fillings and minor replacement and breccia bodies. The paragenetic sequence encompasses four mineralization stages starting with the early high-sulfidation assemblage pyrite + chalcopyrite + enargite-luzonite ± bornite with a continuous transition into intermediate-sulfidation state assemblages comprising pyrite + chalcopyrite + tennantite-tetrahedrite ± electrum ± Ag-bearing sulfosalts. The late paragentic stage with sphalerite + galena + pyrite ± electrum overprints the earlier ones. Supergene mineralization with chalcocite + covellite + Fe-oxyhydroxides + Cu-carbonate hydroxides is restricted to the shallow weathered part of the deposit. A regional zoning of ore minerals is apparent; central parts of the deposit are dominated by Cu-Fe-rich sulfides showing a transition to Pb-Zn-dominated zones mainly in the deeper and distal sections. Variations in the chemical composition of fahlores range from Fe-bearing tennantite to Zn-rich tetrahedrite with a strong positive correlation between Sb and Ag contents. The fahlores are complexly zoned and display a progressive increase of Sb concentration with increasing distance to the nearby Meiduk deposit. Primary fluid inclusions in mineralized O-type veins are low saline aqueous H2O-salt inclusions. They yield homogenization temperatures (Th LV->L) between 115 to 295 °C for sphalerite and 145 to 397 °C for quartz. Salinity values range between 1.2 to 9.9 and 2.1 to 9.2 wt% NaCl equiv., respectively. Raman spectroscopy confirms low CO2 concentrations of the vapor phase of the fluid inclusions. The fluids are interpreted to be of magmatic origin as indicated by previously published stable isotope studies. We propose that ascending cooling magmatic fluids were responsible for the transport of metals and mineral precipitation occurred in the epithermal regime upon dilution of magmatic fluids with meteoric water. Similar low-salinity, CO2-bearing fluids were reported from the nearby Meiduk deposit. Conclusively, Chah-Mesi is classified as an intermediate-sulfidation epithermal deposit with a genetic link to the Meiduk porphyry (Cu-Au) deposit. Mineralization is inferred to hydrothermal fluids with an initial high-sulfidation state, which changed into intermediate-sulfidation state during cooling, dilution and fluid-wallrock interaction.