Chahar-Gonbad copper mine, in Kerman province, has mainly
formed as veins with low reserves and medium grade. Mineralization is
mainly occured as chalcopyrite, pyrite, rare galena and sphalerite. Sericitic,
argillic and propylitic alterations have been identified in this are deposit.
These alteration occurod in the thermal range of about 350 C. In this
research, the morphology of pyrite crystals is used for determination of the
thermal range of mineralization. It is possible that the pyrite form in a
mineralization zone shows the state of thermal range during mineralizaton.
Based on this assumptian, the needle crystals are formed in temperatures
below or equal to 250 C, abundant grooves while with increasing
temperature to 450 C the cubic crystals with abundant grooves and a few
octahedral surfaces are formed. Investigations of collected pyrite crystals
from alteration zones of this ore deposit show that the cubic types with
abundant pyritohedron surfaces are common and crystals with high density
with groove surfaces are seen with smooth surfaces crystals. Therefore it is
interpreted that pyrites have formed in the thermal range between 250 to
450 C. According to the temperature range for alteration (mean 350 C), it
seems copper that the mineralization have occurred between 350 to 450 C.