University of Isfahan Petrological Journal 2228-5210 11 2 2020 08 22 Geochemical data as a tool for estimation of mineralization potential in the Hanar granitoids as part of Tertiary plutonism in Lut block (East of Iran) Geochemical data as a tool for estimation of mineralization potential in the Hanar granitoids as part of Tertiary plutonism in Lut block (East of Iran) 19 36 25423 10.22108/ijp.2020.114566.1114 FA Siavash Omidianfar Department of geology, Faculty of earth science, University of shahid Beheshty, Tehran, Iran Mohammad Rahgoshay استان تهران-شهر تهران- بزرگراه شهید چمران - خیابان اتابک - میدان شهید شهریاری - دانشگاه شهید بهشتی - دانشکده علوم زمین Iman Monsef Graduate University in Basic Sciences Zanjan Journal Article 2018 12 15 Hanar intrusion located in 155 km South of Birjand in the east of Lut block and compositionally consist of tonalite, granodiorite, quartz-diorite and diorite that intruded as stock and dikes in volcanic sequence (basic to intermediate) outcropped in this area. Hanar granitoid rocks are metaluminous and show I-type granitoids affinity. In addition, they are belong to calk-alkaline series and reveal the active continental margin geochemical evidences. According to relation of studying intrusion to I type granitoids with oxide (magnesian) state, they have no potential to produce Sn and W mineralization. Also, Low Sr/Y and V/Sc ratios as well as the situation of the studying samples in barren domain of the fertile-barren discrimination diagrams show that Hanar granitoids have no potential for Cu porphyry mineralization. In other hand, Low degree of the magmatic evolution as well as location of the studying samples in different Fe-mineralization potential evaluation diagrams indicate that Hanar granitoids (Diorite unit) has high potential for formation of iron deposits that this case is supporting by occurrence of  Fe-mineralization (as vein-Iron deposit) in association with this intrusion. <strong> </strong> Hanar intrusion located in 155 km South of Birjand in the east of Lut block and compositionally consist of tonalite, granodiorite, quartz-diorite and diorite that intruded as stock and dikes in volcanic sequence (basic to intermediate) outcropped in this area. Hanar granitoid rocks are metaluminous and show I-type granitoids affinity. In addition, they are belong to calk-alkaline series and reveal the active continental margin geochemical evidences. According to relation of studying intrusion to I type granitoids with oxide (magnesian) state, they have no potential to produce Sn and W mineralization. Also, Low Sr/Y and V/Sc ratios as well as the situation of the studying samples in barren domain of the fertile-barren discrimination diagrams show that Hanar granitoids have no potential for Cu porphyry mineralization. In other hand, Low degree of the magmatic evolution as well as location of the studying samples in different Fe-mineralization potential evaluation diagrams indicate that Hanar granitoids (Diorite unit) has high potential for formation of iron deposits that this case is supporting by occurrence of  Fe-mineralization (as vein-Iron deposit) in association with this intrusion. <strong> </strong> https://ijp.ui.ac.ir/article_25423_ac1ff9322ae6cae0b078e26366d6a22a.pdf