Writers : Nakhaei, M., M. H. Karimpour, S.A. Mazaheri, M.R., Heydarian, M.H.,Zarinkoub
Refference : 1st Symposium of Iranian Society of Economic Geology
Publishing Year : 1389

Abstract :

Acidic to intermediate intrusive rocks intruded Paleocene limestone and formed Iron skarn, in Bisheh southeast of Qaleh Zari. The skarns divided into garnet skarn, garnet epidote skarn and scapolite skarn. Most of garnets have distinguished zonation and based on XRD analysis, the main phase of garnet is Andradite. Using the same method of analysis, the type of Scapolite is Marialite. Magnetite is the main Fe mineral which has oxidized to hematite and limonite at the surface. The grade of Fe in Lakh Sefid region (North of Bisheh) is about 40-70%. Besides the Iron, copper mineralization as Malachite was obsereved in East of Bisheh.

Subject List : Iron