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    Post-collisional H-type granitoid magmatism in Central Anatolia and time-space relation with Fe-oxide mineralization
    (MILLPRESS SCIENCE PUBLISHERS, 2003) Kuscu, I; Kuscu, GG; Soylu, M; Eliopoulous, DG
    The 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.