AI Summary & Key Takeaways
AI InsightIn the nort h of Fındıklı the lower part consists of fine-to medium-grained argillaceous sandstone beds containing many fossils of Callovian-Oxfordian age which are also covered by similar cryptocrystalline limestones.
📌 3 Key Takeaways
Abstract
The Upper Jurassic formations within the area studied begin wes t of the village of Dağakçeköy and extend westwards. The lower part consists of conglomerates-sandstones and marls containing shallow marine fauna of Bathonian-Oxfordian age. The upper part consists of light-brownish cryptocrystalline limestones. In the nort h of Fındıklı the lower part consists of fine-to medium-grained argillaceous sandstone beds containing many fossils of Callovian-Oxfordian age which are also covered by similar cryptocrystalline limestones.
Özet
Mevzuubahis mevkilerdeki Üst Jura formasyonları Dağakçeköy'ün batısında; altta Bathonien-Oksfordien yaşındaki sığ deniz fosillerini ihtiva eden konglomera-gre ve marnlarla, bunun üzerine aflöre eden bej renkli kriptokristalin kalkerlerden; Fındıklı kuzeyinde ise, Kallovien-Oksfordien yaşında bol fosilli, küçük ve orta taneli (fine- to medium-grained) grelerle, yine bunların üzerinde bulunan gri renkli kriptokristalin kalkerlerden müteşekkildir.