Geology, mineralization, zircon U-Pb geochronology and Hf isotopes of Serenu porphyry copper prospect, Kerman Cenozoic magmatic arc, southeastern Iran

Serenu porphyry copper prospect is situated 22 km northwest of the Meiduk copper mine, Kerman Cenozoic magmatic arc in southeastern Iran. The study area is characterized by a simple lithology including Eocene volcanic and volcaniclastics, Neogene sediments, and sub-volcanic rocks (Hezar complex) which is intruded by a late Miocene porphyry diorite to quartz-diorite stock that has developed alteration and mineralization in the area. Phyllic, argillic, and propylitic alteration types are well-distributed in the Serenu prospect; potassic alteration is only locally observed. Hypogene mineralization occurs in the Serenu porphyry and the host Eocene volcanic rocks as scattered vein-veinlets, stockworks, and disseminated mineralization related to potassic and phyllic alteration types.The mineralogy and cross-cutting relationships, allow the vein-veinlets to be classified into five groups including (I) magnetite & PLUSMN; quartz, (II) quartz & PLUSMN; magnetite & PLUSMN; chalcopyrite & PLUSMN; pyrite & PLUSMN; chlorite & PLUSMN; anhydrite (III) quartz & PLUSMN; pyrite & PLUSMN; chalcopyrite & PLUSMN; anhydrite, (IV) pyrite, and (V) quartz & PLUSMN; calcite veinlets. Oxide and supergene enriched ores are poorly developed in the area. Zircon U-Pb dating on two samples from the Serenu porphyry provided consistent ages at 9.83 & PLUSMN; 0.4 Ma and 10.2 & PLUSMN; 0.17 Ma (& PLUSMN;2 & sigma;) indicative of late Miocene emplacement of the intrusion. The zircons are characterized by positive & epsilon;Hf (t) values of 8.52 to 12.27 and TDM of 200-370 Ma and a TCDM of 310-590 Ma indicating that they originated from a juvenile mafic and thickened lower crust and depleted mantle-derived magma.The late Miocene age determined for the Serenu porphyry copper prospect is consistent with the ages reported for many other shallow intrusions related to porphyry-type mineralization in the Kerman belt and further emphasizes the Miocene metallogenic epoch as the preferred time for porphyry Cu-Mo-Au mineralization in this belt, coinciding with a significant stage of continental collision between the Arabian and Iranian plates. The results of this study reveal that the juvenile mafic lower crust together with input from a depleted mantle and older subduction-related magma has a very significant impact on the formation of the Serenu porphyry host magma.