Mineralogy geochemistry and genesis of Kehdolan copper deposit Bostanabad east Azarbaijan
Subject Areas :Alireza Yousefi 1 , Sh. Niroomand 2 * , Abdorrahman Rajabi 3 , mohammad amini 4
1 -
2 - University of Tehran
3 - University of tehran
4 -
Keywords: mineralization, geochemical, alteration, Kehdolan copper, Bostanabad,
Abstract :
Study area is located in Eastern Azerbaijan province, 27 km far from east Bostanabad, and the north of Qarehchaman geological map. According to field tracking and surveys, host rock of mineralization is a Subvolcanic rocks of Oligocene period. Based on microscopic studies, the most important of supergene part, containing primary oxide minerals (Magnetite), secondary oxide minerals (Malachite, Hematite and Goethite) and also sulphide minerals such as Chalcocite, Covellite, Pyrite and insignificance Chalcopyrite. Among the most important alterations, argillic, silicification, carbonization and propylithic can be noted. Geochemical studies shows that host rock of mineralization with Monzosyenitic composition, placed in high chalc-alkaline to shoshonitic and metaluminous range. Formation environment of host rock of mineralization is a volcanic arc of subduction zone that confirmed by normalized rare earth elements diagrams.
- روان¬خواه, موءید, لطفی¬ بخش (1399). مطالعات زمین¬شناسی، دگرسانی و کانی¬سازی کانسار مس پورفیری بارملک (شمال ورزقان-استان آذربایجان¬شرقی). فصلنامه زمین¬شناسی ایران, 56 (75-86).
-حیدری، م. زراسوندی، ع.رضایی، م. ع، ساکی و اسدی، س. (1397). بازسازی شاخص¬های فیزیکوشیمیایی با استفاده از شیمی و کلریت در کانسار مس پورفیری کدر، کمان ماگمائی سنوزوئیک کرمان. فصلنامه زمین شناسی ایران، 47 (63-85).