Middle-Upper Miocene aged borate deposits in the Kırka basin having volcano sedimentary lacustrine rocks are found within
the dolomitic claystone/marls as lense shaped. The most lower and upper parts of the deposit are surrounded by carbonaceous rocks. Borate
deposits situated in the two parts of the region were separated by paleotopographic threshold consisting of basement rocks and/or vertical
blocking movements. Borate minerals show vertical and lateral mineralogical zonation such as Na, NaCa and Ca-borate in the southeastern
area of the basin (Sarıkaya), whereas Ca-borate is represented only in the northwestern area (Göcenoluk). Borate minerals were formed by
different processes such as synsedimentary, authigenesis and diagenetic transformation, according to their shapes/forms and kinds.
Birincil Dil | İngilizce |
---|---|
Konular | Mühendislik |
Bölüm | Makaleler |
Yazarlar | |
Yayımlanma Tarihi | 1 Haziran 1991 |
Yayımlandığı Sayı | Yıl 1991 Cilt: 113 Sayı: 113 |
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