The Neoproterozoic basement and the Early Cambrian units are widely exposed around the Karaçat Iron Deposit and its surrounding, which are located at the eastern part of Tauride-Anatolide platform. The main mineralization was detected as hematite in all deposits in the study area. The ore microscopy, SEM and EDX studies show that carbonate pseudomorphs in hematite have developed and their chemical compo- sitions are enriched in Ca, Mg, Fe, C and O elements. The geochemical analyses of hematite and siderite minerals reveal that both ore mineral types have similar patterns of Rare Earth Element (REE). These data and field observations reveal that hematite is the replacement product after sedimentary siderite minerali- zation. The genesis of the hematite mineralization that is effective over large areas and widely observed on the basement and overlying units, was formed during Late Neoproterozoic- Early Cambrian volcanism in the region defined as Peri-Gondwana. They are genetically described as volcano syn-sedimentary and/or exhalative syn-sedimentary type mineralization.
Iron Mineralization Karaçat Iron Deposit Mansurlu Exhalative Syn-Sedimentary
Birincil Dil | İngilizce |
---|---|
Konular | Mühendislik |
Bölüm | Makaleler |
Yazarlar | |
Yayımlanma Tarihi | 25 Mayıs 2016 |
Yayımlandığı Sayı | Yıl 2016 Cilt: 152 Sayı: 152 |
Copyright and Licence
The Bulletin of Mineral Research and Exploration keeps the Law on Intellectual and Artistic Works No: 5846. The Bulletin of Mineral Research and Exploration publishes the articles under the terms of “Creatice Common Attribution-NonCommercial-NoDerivs (CC-BY-NC-ND 4.0)” licence which allows to others to download your works and share them with others as long as they credit you, but they can’t change them in any way or use them commercially.
For further details;
https://creativecommons.org/licenses/?lang=en