Writers : Ghavi,Jamal;Kalagari,Aliasghar;Karimpour,Mohammadhasan;Saadat,Saeed
Refference : 10th Symposium of Geological Society of Iran-Tehran
Publishing Year : 1385

Abstract :

Study area is located in Eastern section of Volcano-Plutonic Belt in north Duroneh fault.at northeast of Iran. The main characteristics of the area are existence of Palegene volcano-sediment complex and in vast formaticn Oligocene-Neogene detrital sediments. Magrnatisrn activity is in form Paleocene-Eocene volcanic and pyroclastic rocks by intermediates composition and subsequent intruded plutonic and subvolcanic bodies by felsic composition are outcrop. Mainly structure feature in area is fractures in trended and parallel to Duroneh fault system. Putting together geophysical exploration data and consider geochemical data has shown mineralization zones of iron, copper and other associated elements as well as confirm by hammer prospecting. Base on results in paper and comparison data with mineralization models, mineralization pattern in study area are show characteristic Iron oxide mineralization type.

Subject List : Mineralization