Men are the reflection of thoughts in their subconscious.
To start, first you have to believe that you can, then proceed with passion.
Facies structural geology and exploration area and related areas are very complex in nature. Deposits in the vicinity of a complex volcanic - sedimentary Eocene there by tuffs, conglomerates andesite and dacite, tuff, and limestone conglomerate, and limestone oligomiocene altered dacite have been replaced. The main host rock mineralization of copper, shear tuff containing quartz veins rich in iron oxide (gossan) located at the contact of volcanic - sedimentary and igneous rocks.
Copper-Iron exploration area with 1 square kilometers is located in the Kerman province and 30 km south-west Bardsir .Much of Chahar Gonbad plates by the Cenozoic strati graphic units of the Eocene specifically covered. Similarly, within the forty tons of pyroclastic deposits and volcanic rocks show the greatest expansion. Pyroclastic rocks are widespread in parts of northern, central and southern regions are exposed. This unit includes a sequence of fine-grained tuff and agglomerate.The chemical composition of these rocks is generally intermediate to acidic.