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AI Summary & Key Takeaways
AI Insight⚡ TL;DR(Too Long; Didn't Read)
The tectonic îinaments of the region extend in NE-SW and NW-SE direetions.
📌 3 Key Takeaways
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Objective & Hypothesis:In ıhe investigated area successive deformations are exhibiıed in the Upper Creta- ceous-Miocene series due to the subduction and Continental collision in the Northern branch of Ncotethys.
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Key Findings & Data:Four deformational stages (D 1-4) can be recognized in the series, the first two (Dİ—2) of which may represent the independent events.
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Conclusion & Impact:The tectonic îinaments of the region extend in NE-SW and NW-SE direetions.
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:CRETACEOUSTERTIARY · VILLAGES-NORTHWEST · DEFORM
Abstract
In ıhe investigated area successive deformations are exhibiıed in the Upper Creta- ceous-Miocene series due to the subduction and Continental collision in the Northern branch of Ncotethys. Four deformational stages (D 1-4) can be recognized in the series, the first two (Dİ—2) of which may represent the independent events. The main deformation (D3) takes place towards the end of Mid-Miocene time in this period due to Continental collision, Last stage affected the previous struetures as the late events of D3. The tectonic îinaments of the region extend in NE-SW and NW-SE direetions.
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Cite This Article
Gökten, E. (1986). DEFORM A TIONAL STAGES OF THE UPPER CRETACEOUSTERTIARY ROCKS IN THE AREA AROUND ORHANİYE AND MEMLÎK VILLAGES-NORTHWEST ANKARA. Communications Faculty of Sciences University of Ankara Series C Biology, Volume: 04 (1986) Issue: 01.02. https://doi.org/10.1501/Commuc_0000000081