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Geochemical characteristics of iron ore deposits in central eastern Turkey: an approach to their genesis

dc.contributor.authorCansu, Zeynep
dc.contributor.authorKasapci, Cem
dc.contributor.authorHanilci, Nurullah
dc.contributor.authorOzturk, Huseyin
dc.date.accessioned2021-03-04T12:04:57Z
dc.date.available2021-03-04T12:04:57Z
dc.date.issued2016
dc.identifier.citationOzturk H., Kasapci C., Cansu Z., Hanilci N., "Geochemical characteristics of iron ore deposits in central eastern Turkey: an approach to their genesis", INTERNATIONAL GEOLOGY REVIEW, cilt.58, sa.13, ss.1673-1690, 2016
dc.identifier.issn0020-6814
dc.identifier.otherav_75a00908-99e4-4321-baee-caa056b57eea
dc.identifier.othervv_1032021
dc.identifier.urihttp://hdl.handle.net/20.500.12627/80778
dc.identifier.urihttps://doi.org/10.1080/00206814.2016.1183236
dc.description.abstractEconomically the most important iron deposits of Turkey occur as: (1) skarn-hosted (SH)-type ore deposits, occurring along the contacts between syenitic-monzonitic intrusives and limestone or serpentine; (2) vein-type deposits, found between the serpentine and limestone (SLH); or (3) ore deposits that are entirely within the limestone (LH).
dc.language.isoeng
dc.subjectTemel Bilimler (SCI)
dc.subjectMühendislik ve Teknoloji
dc.subjectJEOLOJİ
dc.subjectYerbilimleri
dc.subjectJeoloji Mühendisliği
dc.titleGeochemical characteristics of iron ore deposits in central eastern Turkey: an approach to their genesis
dc.typeMakale
dc.relation.journalINTERNATIONAL GEOLOGY REVIEW
dc.contributor.departmentİstanbul Üniversitesi , ,
dc.identifier.volume58
dc.identifier.issue13
dc.identifier.startpage1673
dc.identifier.endpage1690
dc.contributor.firstauthorID227186


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