Kuscu, IKuscu, GGSoylu, MEliopoulous, DG2019-08-012019-08-01200390-77017-77-1https://hdl.handle.net/11480/57227th Biennial SGA Meeting -- AUG 24-28, 2003 -- Athens, GREECEThe distribution, in both space and time, of the mineral deposits of the Central Anatolia reveals some interesting and enigmatic features of mineralization in a collision related setting. Central Anatolia is a polymetallic metallogenic province hosting mineral deposits of various size and type. Present study concerns with the formation and distribution of the Fe-oxide mineralization in terms of granite metallogeny, and reveals the genetic coexistence of H-type post-collisional granitoid magmatisin and Fe-oxide mineralization.eninfo:eu-repo/semantics/closedAccessCentral AnatoliaFe-oxideCu-AuFe-oxide-Cu-Aupost-collisional H-type magmatismConference Object307310WOS:000221378600076N/A