Stratigraphy and tectono-sedimentary evolution of the Upper Cretaceous–Tertiary sequence in the southern part of the Malatya Basin, East Anatolia, Turkey
Yazarlar (2)
Prof. Dr. Mehmet Mustafa ÖNAL Türkiye
Meral Kaya
Kırşehir Ahi Evran Üniversitesi
Kırşehir Ahi Evran Üniversitesi
| Makale Türü |
Özgün Makale
(Uluslararası alan indekslerindeki dergilerde yayınlanan tam makale)
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| Dergi Adı | Journal of Asian Earth Sciences | ||
| Makale Dili | – | Basım Tarihi | 03-2007 |
| Cilt / Sayı / Sayfa | 29 / 5 / 878–890 | DOI | – |
| Makale Linki | https://www.sciencedirect.com/science/article/pii/S1367912006001714 | ||
| UAK Araştırma Alanları |
Betonarme Yapılar
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| Özet |
| The Malatya Basin is situated on the southern Taurus-Anatolian Platform. The southern part of the basin contains a sedimentary sequence which can be divided into four main units, each separated by an unconformity. From base to top, these are: (1) Permo-Carboniferous; (2) Upper Cretaceous–Lower Paleocene, (3) Middle-Upper Eocene and (4) Upper Miocene. The Upper Cretaceous–Tertiary sedimentary sequence resting on basement rocks is up to 700m thick. The Permo-Carboniferous basement consist of dolomites and recrystallized limestones. The Upper Cretaceous–Lower Paleocene transgressive–regressive sequence shows a transition from terrestrial environments, via lagoonal to shallow-marine limestones to deep marine turbiditic sediments, followed upwards by shallow marine cherty limestones. The marine sediments contain planktic and benthic foraminifers indicating an upper Campanian … |
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