SavedAdd your journal

Journals / Konya Journal of Engineering Sciences / 2023 / Cilt: 11 Sayı: 3

Microfacies and Biofacies Properties of the Lower-Middle Visean Succession of Hadim Nappe (Central Taurides, Southern TÜRKİYE)

HADİM NAPI ALT-ORTA VİZEYEN İSTİFİNİN MİKROFASİYES VE BİYOFASİYES ÖZELLİKLERİ (ORTA TOROSLAR, GÜNEY TÜRKİYE)

Melikan AKBAŞ
Pages
693–705
Publication Date
2023-09-01
DOI
—
🏛️Bibliographic metadata and full text access for this article are provided via DergiPark.
DergiPark Record ↗
✨

AI Summary & Key Takeaways

AI Insight
⚡ TL;DR(Too Long; Didn't Read)

The foraminiferal fauna of the lower-middle Viséan carbonates, which generally indicates stable depositional environments, are adversely affected by minor changes in the depositional environments.

📌 3 Key Takeaways

🎯
Objective & Hypothesis:The Hadim Nappe, which is one of the allochthonous tectono-stratigraphic unit of the Taurides, has a complete succession includes Middle(?)-Upper Devonian-Upper Cretaceous shallow marine carbonates and terrigenous rocks.
📊
Key Findings & Data:According to the microfacies analyses of the lower-middle Viséan succession of the Bademli stratigraphic section, where the Hadim Nappe was well exposed, seven microfacies, which are inditacing Inner Platform Shoal, Restrict and/or Open Marine depositional environments, were indentified.
💡
Conclusion & Impact:The foraminiferal fauna of the lower-middle Viséan carbonates, which generally indicates stable depositional environments, are adversely affected by minor changes in the depositional environments.
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:Toroslar · Hadim Napı · Vizeyen

Abstract

The Hadim Nappe, which is one of the allochthonous tectono-stratigraphic unit of the Taurides, has a complete succession includes Middle(?)-Upper Devonian-Upper Cretaceous shallow marine carbonates and terrigenous rocks. According to the microfacies analyses of the lower-middle Viséan succession of the Bademli stratigraphic section, where the Hadim Nappe was well exposed, seven microfacies, which are inditacing Inner Platform Shoal, Restrict and/or Open Marine depositional environments, were indentified. These are; Bioclastic Grainstone, Bioclastic Grainstone-Packstone, Sandy Bioclastic Grainstone, Sandy Bioclastic Grainstone-Packstone, Bioclastic Pelloidal Grainstone, Bioclastic Wackestone and Sandstone microfacies. The identified microfacies have diverse and rich foraminiferal fauna based on the biofacies analyses. The foraminiferal fauna of the lower-middle Viséan carbonates, which generally indicates stable depositional environments, are adversely affected by minor changes in the depositional environments.

Özet

Toroslar’daki allokton tektono-stratigrafik birimlerden biri olan Hadim Napı Orta(?)-Üst Devoniyen-Üst Kretase sığ platform karbonatları ve kırıntılı kayaçlardan oluşan kesintisiz bir istife sahiptir. Hadim Napı’nın iyi yüzeylendiği Bademli stratigrafik kesiti alt-orta Vizeyen istifinin mikrofasiyes incelemeleri sonucunda İç Platform Kıyı, Sınırlı ve/veya Açık Deniz depolanma ortamlarını yansıtan yedi mikrofasiyes tanımlanmıştır. Bunlar; Biyoklastik Tanetaşı, Biyoklastik Tanetaşı-İstiftaşı, Kumlu Biyoklastik Tanetaşı, Kumlu Biyoklastik Tanetaşı-İstiftaşı, Biyoklastik Pelloidal Tanetaşı, Biyoklastik Vaketaşı ve Kumtaşı mikrofasiyesleridir. Tanımlanan mikrofasiyeslerin yapılan biyofasiyes incelemelerine göre genel olarak zengin bir çeşitlilik ve bolluk sunan foraminifer faunasına sahip olduğu görülmektedir. Genel olarak stabil bir depolanma ortamını işaret eden alt-orta Vizeyen karbonatlarındaki foraminifer faunasının depolanma ortamındaki ufak değişimlerden olumsuz olarak etkilendiği görülmektedir.

🔖

Cite This Article

AKBAŞ, M. (2023). Microfacies and Biofacies Properties of the Lower-Middle Visean Succession of Hadim Nappe (Central Taurides, Southern TÜRKİYE). Konya Journal of Engineering Sciences, Cilt: 11 Sayı: 3, 693–705. https://ajindex.com/articles/964589

📄 Full Text PDF Viewer

📄

PDF görüntüleyici hazırlanıyor...

References (8)

  1. J.L. Isbell, M.F. Miller, K.L. Wolfe, P.A. Lenaker, “Timing of Late Paleozoic glaciation in Gondwana: was glaciation responsible for the development of Northern Hemisphere cyclothems?: Extreme depositional environments: mega end members in geologic time,” Eds.: M.A. Chan, A.W. Archer, Geological Society of America, Boulder, Colorado, special paper, vol. 370, pp 5–24, 2003. I.P. Montañez, C.J. Poulsen, “The Late Paleozoic ice age: an evolving paradigm,” Annual Review of Earth and Planetary Sciences, vol. 41, pp. 629–656, 2013.
  2. E.L.M. Rosa, J.L. Isbell, “Late Paleozoic glaciation,” Encyclopedia of Geology, 2nd edition, Eds: D. Alderton, S.A. Elias, Elsevier, Amsterdam, pp 534–345, 2020.
  3. E.L. Grossman, P. Bruckschen, H.S. Mii, B.I. Chuvashov, T.E. Yancey, J. Veizer, “Carboniferous paleoclimate and global change: isotopic evidence from the Russian Platform: Carboniferous stratigraphy and paleogeography in Eurasia,” Institute of Geology and Geochemistry, Russian Academy of Sciences, Urals Branch, Ekaterinburg, pp 61–71, 2002.
  4. E.L. Grossman, T.E. Yancey, T.E. Jones, P. Bruckschen, B.I. Chuvashov, S.J. Mazzullo, H.S. Mii, “Glaciation, aridification, carbon sequestration in the Permo-Carboniferous: the isotopic record from low latitudes,” Palaeogeography, Palaeoclimatology, Palaeoecology, Vol. 268, pp. 222–233, 2008.
  5. C.R. Fielding, T.D. Frank, L.P. Birgenheier, M.C. Rygel, A.T. Jones, J. Roberts, “Stratigraphic imprint of the Late Palaeozoic ice age in eastern Australia: a record of alternating glacial and non-glacial climate regime,” Journal of the Geological Society of London, vol. 165, no. 1, pp. 129–140, 2008a.
  6. C.R. Fielding, T.D. Frank, L.P. Birgenheier, M.C. Rygel, A.T. Jones, J. Roberts, “Stratigraphic record and facies associations of the Late Paleozoic ice age in eastern Australia (New South Wales and Queensland): Resolving the Late Paleozoic Ice Age in time and space,” Eds.: C.R. Fielding, T.D. Frank, J.L. Isbell, Geological Society of America Special Paper, vol. 441, pp. 41–57, 2008b.
  7. C.R. Fielding, T.D. Frank, J.L. Isbell, “The Late Paleozoic ice age—a review of current understanding and synthesis of global climate patterns: Resolving the Late Paleozoic Ice Age in time and space,” Eds.: C.R. Fielding, T.D. Frank, J.L. Isbell, Geological Society of America Special Paper, vol. 441, pp. 343–354, 2008c.
  8. W. Buggisch, X. Wang, A.S. Alekseev, M.M. Joachimski, “Carboniferous-Permian carbon isotope stratigraphy of successions from China (Yangtze platform), USA