پتانسیلهای معدنی ورقه دیزج با نگرشی ویژه بر پتانسیلهای سنگهای افیولیت ملانژ

                The study area located in northwest of Iran and in southern part of Dizag ۱ : ۱۰۰۰۰۰ map sheet. From the geological point of view the above mentioned area is in western Alborz Structural Zone – Azarbaijan ( Nabavi, ۱۹۷۶ ) and NW Colored melange unit ( Khoy ; Khoy – Mahabad zone ) including of different rocks such as:              ۱) metamorphic rocks, schists, amphibolite and marble ۲) ophiolitic rocks including dunite, harzburgite and  lisvenite ۳) pillow lavas ۴) plagic limestone and sedimentary rocks  such as shale, sandstone on Cretaceous and Paleocene limestone. Au anomaly in siliceous lisvenite and Mn deposite accompany with Fe oxide in pillow lava and Cr deposite, Ni and Co anomalies in hurzburgite host rocks and serpantinized dunite can be indicated as valuable mineral potential in these rocks.