Geology and trona potential of the middle Miocene Gürün (Sivas) basin, Central Anatolia, Turkey
Yazarlar (3)
| Makale Türü | Özgün Makale (Uluslararası alan indekslerindeki dergilerde yayınlanan tam makale) | ||
| Dergi Adı | Carbonates and Evaporites | ||
| Makale Dili | – | Basım Tarihi | 01-2004 |
| Cilt / Sayı / Sayfa | 19 / 2 / 118–132 | DOI | 10.1007/BF03178475 |
| Makale Linki | https://link.springer.com/article/10.1007/BF03178475 | ||
| UAK Araştırma Alanları |
Betonarme Yapılar
|
||
| Özet |
| Gürün (Sivas) basin, extending along east-west direction, contains a volcano-sedimentary sequence of up to 1222 m thick. The middle Miocene sedimentary sequence rest with angular unconformity on the basement rocks, which consist of limestone and flysch sediments ranging in Triassic-Jurassic-Cretaceous and middle-upper Eocene. The sequence has been subdivided into Gürün Formation and Karadaĝ Volcanics. The Gürün Formation consist of four members in ascending order: Kavak, Gökpinar, Çayboyu and Terzioĝlu members. Trona occurences are placed within the Terzioĝlu member, alternating with bituminous shale, mudstones and tuffs; whereas the lignite deposits occured in the Çayboyu member of the Gürün Formation.The Miocene sedimentary rock units are laterally and vertically gradational. Karadaĝ volcanics, located in the eastern and northern parts of basin, interfinger with the upper parts of … |
| Anahtar Kelimeler |
BM Sürdürülebilir Kalkınma Amaçları
| Atıf Sayıları | |
| Google Scholar | 21 |