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 (SCI-Expanded, Scopus)
- Yayın Türü: Makale / Tam Makale
- Cilt numarası: 58 Sayı: 13
- Basım Tarihi: 2016
- Doi Numarası: 10.1080/00206814.2016.1183236
- Dergi Adı: International Geology Review
- Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
- Sayfa Sayıları: ss.1673-1690
- Anahtar Kelimeler: Iron ore deposits, geochemistry, element association, central eastern Anatolides, Turkey, RARE-EARTH-ELEMENTS, KIRUNA-TYPE, CENTRAL ANATOLIA, APATITE, MAGNETITE, SWEDEN, EVOLUTION, OXYGEN, MINERALIZATION, GEOCHRONOLOGY
- İstanbul Üniversitesi-Cerrahpaşa Adresli: Hayır
Özet
Economically 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).