جدایش بی‌هنجاری‌های عناصر، بر پایه داده‌های ژیوشیمی سطحی خاک در کانسار مس ‏پورفیری کهنگ– شمال خاوری اصفهان

The kahang copper porphyry deposit on urumieh-dokhtar magmatic arc, is located in ne of esfahan. around of this deposit, eocene ‎volcanics and pyroclastic rocks ranging in composition from basaltic trachy-andesitic to dacitic are exposed. granitoids subvolcanic and ‎volcanoplutonic, the causes of alteration and mineralizaton, replacement in eocene rocks assemblage in afew puls from oligocene to ‎miocene. this plutons ranging in composition from monzodiorite quartzdiorite granodiorite to granite with porphyroeidal texture. alteration ‎and mineralization is classically developed in this deposit. samples from surface soil were collected in 50m profiles gridding which the ‎distance samplings in along the profile are 25m. the total numbers of samples are 2564 which are analyzed by icp-oes method for 43 ‎elements. in geochemical anomaly maps, activating of faults with another tectonic factors, environmental conditions alteration and erosion in ‎moving and concentration this anomaly are illustrated. same as the litho geochemical anomalies the most amount distribution of cu in the ‎eastern and center of the region, au in the west and center and mo in all three region are depicted. in elemental correlation graphs suitable ‎correlation is for copper and gold.‎