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

Ozturk H., Kasapci C., Cansu Z., Hanilci N.

INTERNATIONAL GEOLOGY REVIEW, cilt.58, sa.13, ss.1673-1690, 2016 (SCI-Expanded) identifier identifier

  • 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
  • İstanbul Üniversitesi Adresli: Evet

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).