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Tuzgölü Havzasından Üst Eosen-Oligosen kumtaşlarının jeokimyası (Orta Anadolu)

Yıl 2022, Cilt: 11 Sayı: 1, 157 - 169, 14.01.2022
https://doi.org/10.28948/ngumuh.1018818

Öz

Bu çalışmada, Tuzgölü Havzasının doğu sınırında Tuzgölü Fay Zonu (TFZ) tarafından açığa çıkarılmış olan Üst Eosen-Oligosen kumtaşlarının mineralojik ve jeokimyasal özellikleri incelenmiştir. Th/Sc-Zr/Sc diyagramında zirkon zenginleşmesinin olmaması, sedimanter tekrardan çevrim olmadığını belirtmiştir. Bu, kumtaşlarının birinci döngü çökel olduğunu yani malzemenin doğrudan kaynaktan gelmiş olduğunu göstermektedir. La/Sc, La/Co, Th/Sc, Th/Co, Th/Cr, Zr/Sc, Zr/Co, Ba/Sc ve Ba/Co gibi provenans için kritik element oranları, Th/Sc-Eu/Eu* diyagramı ve ortalama Nadir Toprak Element (NTE) deseni, “ortaç magmatik” bileşimli bir provenansı önermektedir. İstifin alt ve üst kısımları arasında gözlemlenen negatif Ce anomalisi etkisindeki farklılık, suyun oksijen seviyesinde değişim olduğunu göstermektedir. La-Th-Sc, Th-Co-Zr/10 ve Th-Sc-Zr/10 tektonik konum ayırma diyagramlarının her birinde kumtaşı ortalaması “Kıtasal Adayayı” konumuna düşmüştür. Bu tektonik konum dalma batma zonunun kıta kenarında gelişen bir yaydır. Bulunan tektonik konum, Tuzgölü Havzasının bir yay önü havza olarak geliştiği yönündeki evrim modelini desteklemiştir.

Destekleyen Kurum

Selçuk Üniversitesi (BAP)

Proje Numarası

09101002

Kaynakça

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  • H. Ü. Ercan, M. Ç. Karakaya, A. Bozdağ, N. Karakaya and A. Delikan, Origin and evolution of halite based on stable isotopes (δ37Cl, δ81Br, δ11B and δ7Li) and trace elements in Tuz Gölü Basin, Turkey. Applied Geochemistry, 105, 17-30, 2019. https://doi.org/10.1016/j.apgeochem.2019.04.008.
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Geochemistry of Upper Eocene-Oligocene sandstones from Tuzgölü Basin (Central Anatolia)

Yıl 2022, Cilt: 11 Sayı: 1, 157 - 169, 14.01.2022
https://doi.org/10.28948/ngumuh.1018818

Öz

In this study, mineralogical and geochemical features of Upper Eocene-Oligocene sandstones exposed by the Tuzgölü Fault Zone (TFZ) at the eastern border of the Tuzgölü Basin were investigated. The absence of zircon enrichment in the Zr/Sc-Th/Sc diagram indicated no sedimentary recycling. This shows that the sandstones are first cycle sediments, that is, the material transported directly from the source. Critical element ratios for provenance such as La/Sc, La/Co, Th/Sc, Th/Co, Th/Cr, Zr/Sc, Zr/Co, Ba/Sc, and Ba/Co, Th/Sc-Eu/Eu* diagram and average Rare Earth Element (REE) pattern suggest a provenance in “intermediate magmatic” composition. The variation in the negative Ce anomaly effect observed between the lower and upper parts of the sequence indicates variation in the oxygen level of the water. In each of the La-Th-Sc, Th-Co-Zr/10, and Th-Sc-Zr/10 tectonic setting discrimination diagrams, the sandstone average fell onto the “Continental Island Arc” position. This tectonic setting defines the arc that developed along the continental margin of the subduction zone. The tectonic setting found for the basin, supported the evolution model that the Tuzgölü Basin developed as a fore-arc basin.

Proje Numarası

09101002

Kaynakça

  • A. Aydemir, Hydrocarbon potential of the Tuzgolu (Salt Lake) Basin, Central Anatolia, Turkey: A comparison of geophysical investigation results with the geochemical data. Journal of Petroleum Science and Engineering, 61 (1), 33-47, 2008. http://dx.doi.org/ 10.1016/j.petrol.2007.10.004
  • A. Aydemir, Tectonic investigation of Central Anatolia, Turkey, using geophysical data. Journal of Applied Geophysics, 68, 321-334, 2009.
  • A. Aydemir and A. Ateş, Interpretation of Suluklu-Cihanbeyli-Goloren magnetic anomaly, Central Anatolia, Turkey: An integration of geophysical data. Physics of the Earth and Planetary Interiors, 159 (3–4), 167-182, 2006. http://dx.doi.org/10.1016/ j.pepi.2006.06.007
  • C. Gürbüz and J. R. Evans, A seismic refraction study of the western Tuz Gölü basin, central Turkey. Geophysical Journal International, 106 (1), 239-251, 1991. https://doi.org/10.1111/j.1365-246X.1991.tb04614.x.
  • H. Ü. Ercan, M. Ç. Karakaya, A. Bozdağ, N. Karakaya and A. Delikan, Origin and evolution of halite based on stable isotopes (δ37Cl, δ81Br, δ11B and δ7Li) and trace elements in Tuz Gölü Basin, Turkey. Applied Geochemistry, 105, 17-30, 2019. https://doi.org/10.1016/j.apgeochem.2019.04.008.
  • K. Dirik and M. C. Göncüoglu, Neotectonic characteristics of Central Anatolia. International Geology Review, 38 (9), 807-817, 1996. https://doi.org/10.1080/00206819709465363.
  • E. Özsayin and K. Dirik, Quaternary activity of the Cihanbeyli and Yeniceoba fault zones: İnönü-Eskişehir fault system, Central Anatolia. Turkish Journal of Earth Sciences, 16 (4), 471-492, 2007.
  • M. Y. Hüseyinca, Mineralogical and geochemical characteristics of the sediments in Lake Tuz and the close vicinity (in Turkish). Ph.D. Thesis, Selçuk University, Konya, 2015.
  • A. Uygun and E. Şen, Tuz Gölü Havzası ve doğal kaynakları I: Tuz Gölü suyunun jeokimyası. Bulletin of the Geological Society of Turkey, 21, 113-120, 1978.
  • K. Dirik and O. Erol, Tuzgölü ve civarının tektonomorfolojik evrimi Orta Anadolu, Türkiye. Türkiye Petrol Jeologları Derneği Özel Sayı, 5, 27-46, 2000.
  • M. Clark and A. Robertson, The role of the Early Tertiary Ulukisla Basin, southern Turkey, in suturing of the Mesozoic Tethys Ocean. Journal of the Geological Society, 159 (6), 673-690, 2002.
  • N. Görür, F. Y. Oktay, İ. Seymen and A. M. C. Şengör, Palaeotectonic evolution of the Tuzgölü basin complex, Central Turkey: sedimentary record of a Neo-Tethyan closure. In J. E. Dixon, A. H. F. Robertson (Eds.), The geological evolution of the eastern mediterranean, pp. 467-482, Geological Society Special Publications, London, 1984.
  • A. Koçyiğit, An example of an accretionary forearc basin from northern Central Anatolia and its implications for the history of subduction of Neo-Tethys in Turkey. Geological Society of America Bulletin, 103 (1), 22-36, 1991. https://doi.org/ 10.1130/00167606(1991)103<0022:aeoaaf>2.3.co;2.
  • Y. Arıkan, Tuz Gölü havzasının jeolojisi ve petrol imkanları. M.T.A. Dergisi, 85, 17-38, 1975.
  • I. Çemen, M. C. Göncüoglu and K. Dirik, Structural evolution of the Tuzgölü basin in Central Anatolia, Turkey. The Journal of geology, 107 (6), 693-706, 1999.
  • M. Clark and A. Robertson, Uppermost Cretaceous–Lower Tertiary Ulukışla Basin, south-central Turkey: sedimentary evolution of part of a unified basin complex within an evolving Neotethyan suture zone. Sedimentary Geology, 173 (1), 15-51, 2005. https://doi.org/10.1016/j.sedgeo.2003.12.010.
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Toplam 74 adet kaynakça vardır.

Ayrıntılar

Birincil Dil İngilizce
Konular Mühendislik
Bölüm Jeoloji Mühendisliği
Yazarlar

Mehmet Yavuz Hüseyinca 0000-0003-3863-6170

Suaip Küpeli 0000-0002-3164-6811

Proje Numarası 09101002
Yayımlanma Tarihi 14 Ocak 2022
Gönderilme Tarihi 3 Kasım 2021
Kabul Tarihi 27 Aralık 2021
Yayımlandığı Sayı Yıl 2022 Cilt: 11 Sayı: 1

Kaynak Göster

APA Hüseyinca, M. Y., & Küpeli, S. (2022). Geochemistry of Upper Eocene-Oligocene sandstones from Tuzgölü Basin (Central Anatolia). Niğde Ömer Halisdemir Üniversitesi Mühendislik Bilimleri Dergisi, 11(1), 157-169. https://doi.org/10.28948/ngumuh.1018818
AMA Hüseyinca MY, Küpeli S. Geochemistry of Upper Eocene-Oligocene sandstones from Tuzgölü Basin (Central Anatolia). NÖHÜ Müh. Bilim. Derg. Ocak 2022;11(1):157-169. doi:10.28948/ngumuh.1018818
Chicago Hüseyinca, Mehmet Yavuz, ve Suaip Küpeli. “Geochemistry of Upper Eocene-Oligocene Sandstones from Tuzgölü Basin (Central Anatolia)”. Niğde Ömer Halisdemir Üniversitesi Mühendislik Bilimleri Dergisi 11, sy. 1 (Ocak 2022): 157-69. https://doi.org/10.28948/ngumuh.1018818.
EndNote Hüseyinca MY, Küpeli S (01 Ocak 2022) Geochemistry of Upper Eocene-Oligocene sandstones from Tuzgölü Basin (Central Anatolia). Niğde Ömer Halisdemir Üniversitesi Mühendislik Bilimleri Dergisi 11 1 157–169.
IEEE M. Y. Hüseyinca ve S. Küpeli, “Geochemistry of Upper Eocene-Oligocene sandstones from Tuzgölü Basin (Central Anatolia)”, NÖHÜ Müh. Bilim. Derg., c. 11, sy. 1, ss. 157–169, 2022, doi: 10.28948/ngumuh.1018818.
ISNAD Hüseyinca, Mehmet Yavuz - Küpeli, Suaip. “Geochemistry of Upper Eocene-Oligocene Sandstones from Tuzgölü Basin (Central Anatolia)”. Niğde Ömer Halisdemir Üniversitesi Mühendislik Bilimleri Dergisi 11/1 (Ocak 2022), 157-169. https://doi.org/10.28948/ngumuh.1018818.
JAMA Hüseyinca MY, Küpeli S. Geochemistry of Upper Eocene-Oligocene sandstones from Tuzgölü Basin (Central Anatolia). NÖHÜ Müh. Bilim. Derg. 2022;11:157–169.
MLA Hüseyinca, Mehmet Yavuz ve Suaip Küpeli. “Geochemistry of Upper Eocene-Oligocene Sandstones from Tuzgölü Basin (Central Anatolia)”. Niğde Ömer Halisdemir Üniversitesi Mühendislik Bilimleri Dergisi, c. 11, sy. 1, 2022, ss. 157-69, doi:10.28948/ngumuh.1018818.
Vancouver Hüseyinca MY, Küpeli S. Geochemistry of Upper Eocene-Oligocene sandstones from Tuzgölü Basin (Central Anatolia). NÖHÜ Müh. Bilim. Derg. 2022;11(1):157-69.

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