Journals / Communications Faculty of Sciences University of Ankara Series C Biology / 1986 / Cilt: 04 (1986) - Sayı: 01.02

SEDIMENTARY CHARACTERISTICS OF TERRESTRIAL PALEOCENE DEPOSITS IN NORTHERN ANKARA REGION, TURKEY

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Publication Date
1986-01-01
DOI
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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:Öz 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:Anahtar Kelimeler SEDIMENTARY CHARACTERISTICS · TERRESTRIAL PALEOCENE · NORTHERN

Özet

Öz 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

KAZANCI, N. (1986). SEDIMENTARY CHARACTERISTICS OF TERRESTRIAL PALEOCENE DEPOSITS IN NORTHERN ANKARA REGION, TURKEY. Communications Faculty of Sciences University of Ankara Series C Biology, Cilt: 04 (1986) - Sayı: 01.02. https://ajindex.com/articles/247953

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References (1)

  1. Ankara Üniversitesi – Communications Faculty of Sciences University of Ankara Series C Biology Dergisi