Writers : Nami Nasrabadi,Seid Majid
Refference : The 21st Symposium on Geoscience;Tehran
Publishing Year : 1381

Abstract :

��� Chah poloon mining index is located at 54km in the west of Ferdows(north latitude34 10’ and east latitude 57 45’20’’).
��� From geological situation this area is part of Lut zone and is located at end of its northeast.
��� The oldest outcrop which is observed in the studied area is Cretaceous Limestone which is coverd by the equivalent Kerman Conglomerate;and both are overlined by the volcanic rocks.
��� From structural geology point of view tow fault systems are observed in thestudied area:
1-The major system shows a NE-SW trend and copper(Cu) mineralization has been formed within this system.
2-The minor system with an E-W trend has cut the major faults caused some dislocation within them.
��� Volcanic rock classification shows that rocksfrom older to younger-types include Dacite,Trachydacite,Rhyolite and Andesite.It is be noted that outcrop of green tuff is observed to a limited extent.

Subject List : Copper