Cretaceous-Tertiary (KT) boundary evaporites in the Malatya Basin, eastern Turkey
Yazarlar (5)
Turhan Ayyıldız
Baki Varol
Prof. Dr. Mehmet Mustafa ÖNAL Türkiye
Erdoğan Tekin
İbrahim Gündoğan
Kırşehir Ahi Evran Üniversitesi
Kırşehir Ahi Evran Üniversitesi
| Makale Türü | Özgün Makale (Uluslararası alan indekslerindeki dergilerde yayınlanan tam makale) | ||
| Dergi Adı | Carbonates and Evaporites | ||
| Makale Dili | – | Basım Tarihi | 01-2015 |
| Cilt / Sayı / Sayfa | 30 / 4 / 461–476 | DOI | 10.1007/s13146-015-0254-5 |
| Makale Linki | https://link.springer.com/article/10.1007/s13146-015-0254-5 | ||
| UAK Araştırma Alanları |
Betonarme Yapılar
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| Özet |
| The Malatya basin is situated on the Anatolid-Torid plate of the Neo-Tethys Sea. Evaporites were deposited in the northwestern part of the Malatya basin, which is referred to as the Hekimhan sub-basin. Although the Gündüzbey sub-basin in the southeastern Malatya basin has coeval deposits, it contains no evaporate deposits. The evaporite is most likely the result of the last transgressive–regressive cycle of the Late Cretaceous Sea. The pre-evaporitic unit is represented by the carbonate platform deposit of the Loftusia banks, which partly underwent dolomitization and overlies the deep marine sediments. Celestite-bearing algal limestone was deposited directly below the gypsum-dominated evaporate unit in association with the organic-rich mudstone. Evaporite sedimentation took place in various types of environments, such as marginal shallow subaqueous with the association of sabkha–coastal lagoon and … |
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BM Sürdürülebilir Kalkınma Amaçları
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| Google Scholar | 12 |