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AI Summary & Key Takeaways
AI Insight⚡ TL;DR(Too Long; Didn't Read)
Ali these deposits are in a vertical örder both grain size and depositional environment and they pass into marine Eocene units.
📌 3 Key Takeaways
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Objective & Hypothesis:The terrestrial Paleocene sequences at the north of Ankara are chiefly composed of alluvial fan deposits, braided and meandering river sediments and lacustrine carbonate mudstones.
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Key Findings & Data:In a limited area, only around Orhaniye village, fine-grained volcanoclastics and lavaş are observed.
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Conclusion & Impact:Ali these deposits are in a vertical örder both grain size and depositional environment and they pass into marine Eocene units.
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:SEDIMENTARY CHARACTERISTICS · TERRESTRIAL PALEOCENE · NORTHERN
Abstract
The terrestrial Paleocene sequences at the north of Ankara are chiefly composed of alluvial fan deposits, braided and meandering river sediments and lacustrine carbonate mudstones. In a limited area, only around Orhaniye village, fine-grained volcanoclastics and lavaş are observed. Ali these deposits are in a vertical örder both grain size and depositional environment and they pass into marine Eocene units.
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Cite This Article
Kazancı, N. (1986). SEDIMENTARY CHARACTERISTICS OF TERRESTRIAL PALEOCENE DEPOSITS IN NORTHERN ANKARA REGION, TURKEY. Communications Faculty of Sciences University of Ankara Series C Biology, Volume: 04 (1986) Issue: 01.02. https://doi.org/10.1501/Commuc_0000000083