Post-collisional H-type granitoid magmatism in Central Anatolia and time-space relation with Fe-oxide mineralization

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dc.contributor.authorKuscu, I
dc.contributor.authorKuscu, GG
dc.contributor.authorSoylu, M
dc.contributor.editorEliopoulous, DG
dc.date.accessioned2019-08-01T13:38:39Z
dc.date.available2019-08-01T13:38:39Z
dc.date.issued2003
dc.departmentNiğde ÖHÜ
dc.description7th Biennial SGA Meeting -- AUG 24-28, 2003 -- Athens, GREECE
dc.description.abstractThe 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.
dc.description.sponsorshipSoc Geol Appl
dc.identifier.endpage310
dc.identifier.isbn90-77017-77-1
dc.identifier.startpage307
dc.identifier.urihttps://hdl.handle.net/11480/5722
dc.identifier.wosWOS:000221378600076
dc.identifier.wosqualityN/A
dc.indekslendigikaynakWeb of Science
dc.institutionauthor[0-Belirlenecek]
dc.language.isoen
dc.publisherMILLPRESS SCIENCE PUBLISHERS
dc.relation.ispartofMINERAL EXPLORATION AND SUSTAINABLE DEVELOPMENT, VOLS 1 AND 2
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subjectCentral Anatolia
dc.subjectFe-oxide
dc.subjectCu-Au
dc.subjectFe-oxide-Cu-Au
dc.subjectpost-collisional H-type magmatism
dc.titlePost-collisional H-type granitoid magmatism in Central Anatolia and time-space relation with Fe-oxide mineralization
dc.typeConference Object

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