It is interpreted that the Tertiary sequence of the region was first deposited in a continental and then in a marine environment.
📌 3 Key Takeaways
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Objective & Hypothesis:In the present study, the ostracoda fauna of the sedimentary rocks of Lower Paleogene situated in south of the Polath Town have been stratigraphicaly examined, its biozones have been distinguished and the findings are interpreted from the cronostratigraphic and environmental point of view.
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Key Findings & Data:By evoluating the stratigraphic distribution of 44 ostracoda species, the existance of 4 biozones in Montian—Cuisian have been proposed.
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Conclusion & Impact:It is interpreted that the Tertiary sequence of the region was first deposited in a continental and then in a marine environment.
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:Domain Parameters
Abstract
In the present study, the ostracoda fauna of the sedimentary rocks of Lower Paleogene situated in south of the Polath Town have been stratigraphicaly examined, its biozones have been distinguished and the findings are interpreted from the cronostratigraphic and environmental point of view. By evoluating the stratigraphic distribution of 44 ostracoda species, the existance of 4 biozones in Montian—Cuisian have been proposed. It is interpreted that the Tertiary sequence of the region was first deposited in a continental and then in a marine environment.
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Cite This Article
DURU, M., GÖKÇEN, N. (1990). THE OSTRACODA BIO STRATIGRAPHY AND ENVIRONMENTAL INTERPRETATION OF THE MONTIAN-CUISIAN SEQUENCE IN THE SOUTH OF POLATLI (SW ANKARA). Maden Tetkik ve Arama Dergisi, Cilt: 110 - Sayı: 110, 87–87. https://ajindex.com/articles/54358
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