Journals / Maden Tetkik ve Arama Dergisi / 2019 / Cilt: 158 - Sayı: 158

Factors controlling the paleo-sedimentary conditions of Çeltek oil shale, Sorgun-Yozgat/Turkey

Pages
251–263
Publication Date
2019-04-25
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)

Such variable geochemical conditions in the basin resulted in variable paleo-environmental conditions.

📌 3 Key Takeaways

🎯
Objective & Hypothesis:The study field covering an area of about 1000 km2 is located in Sorgun town of the city of Yozgat.
📊
Key Findings & Data:In order to examine the paleo-sedimentary conditions of oil shales in the study area and their relation to Total Organic Carbon (TOC) contents and major-trace element contents, a total of 29 samples were collected from two boreholes and one Measured Stratigraphic Section (MSS).
💡
Conclusion & Impact:Such variable geochemical conditions in the basin resulted in variable paleo-environmental conditions.
🔬Design:Research Article
📍Scope:29 samples
⚙️Variables:Paleo-environment · paleo- salinity · paleo-climate

Abstract

The study field covering an area of about 1000 km2 is located in Sorgun town of the city of Yozgat. In the region Paleozoic, Campanian-Maastrichtian, Eocene, Miocene and Quaternary units are exposed. Among these units, the lower Eocene Çeltek formation hosts coal beds and oil shale. The Eocene epoch is important for organic matter deposition regarding oil and gas productivity and anoxic depositional conditions. In order to examine the paleo-sedimentary conditions of oil shales in the study area and their relation to Total Organic Carbon (TOC) contents and major-trace element contents, a total of 29 samples were collected from two boreholes and one Measured Stratigraphic Section (MSS). Samples have TOC contents varying from 1.97 to 16.17 wt% (average 6.30 wt%). The V/Cr, V/(V+Ni), U/Th, δU and Authigenic Uranium (AU) values of the Çeltek formation oil shales (ÇFOS) reveal that the oil shales have been deposited under variable paleo-environmental conditions. For paleo-salinity the Sr/Ba ratios indicate mostly deposition in a freshwater environment. Chemical Alteration Index (CIA) values and Sr/ Cu ratios indicate that paleo-climate conditions of ÇFOS were dry, hot and occasionally humid. The Fe/ Ti and (Fe+Mn)/Ti ratios reveal hydrothermal activity during sedimentation of oil shales. Zr/Rb ratios of samples are indicative of very weak paleo-hydrodynamics during the deposition of oil shales. Such variable geochemical conditions in the basin resulted in variable paleo-environmental conditions.

🔖

Cite This Article

PEHLİVANLI, B. Y. (2019). Factors controlling the paleo-sedimentary conditions of Çeltek oil shale, Sorgun-Yozgat/Turkey. Maden Tetkik ve Arama Dergisi, Cilt: 158 - Sayı: 158, 251–263. https://ajindex.com/articles/53923

📄 Full Text PDF Viewer

📄

PDF görüntüleyici hazırlanıyor...

References (11)

  1. Achterberg, E. P., Van Den Berg, C. M. G., Boussemart, M., Davison W. 1997. Speciation and Cycling of Trace Metals in Esthwaite Water: A Productive English Lake With Seasonal Deep-Water Anoxia. Geochim. Cosmochim. Acta,Vol. 61, pp. 5233– 5253. Bai, Y., Liu, Z., Sun, P., Liu R., Hu, X., Zhao, H., Xu, Y., 2015. Rare earth and major element geochemistry of Eocene fine-grained sediments in oil shale- and coal-bearing layers of the Meihe Basin, Northeast China. J Asian Earth Sci., 97, Vol., 97, pp. 89–101.
  2. Beyazpirinç, M., Akçay, A.E., Tarhan, N., Sönmez, M.K., Havzoğlu, T., Bilgiç, T., Bademler, F., Ünal, M. 2014. Akdağmadeni masifi nin jeolojisi ve jeodinamik evrimi projesi 2011-2012 yıllarına ait ara rapor. Maden Tetkik ve Arama Genel Müdürlüğü Rapor No: 11763, Ankara (yayımlanmamış). Boström, K. 1983. Genesis of ferromanganese deposits- diagnostic criteria for recent and old deposits. Hydrothermal Processes at Seafloor Spreading Centers, Springer, Berlin, pp 473–489
  3. Breit, G. N., Wanty, R. B. 1991. Vanadium accumulation in carbonaceous rocks: a review of geochemical controls during deposition and diagenesis. Chemical Geology, Vol. 91, pp. 83-97.
  4. Brumsack, H. J. 2006. The trace metal content of recent organic carbon-rich sediments: Implications for Cretaceous black shale formation; Palaeogeography, Palaeoclimatology, Palaeoecology, Vol. 232, pp. 344–361.
  5. Calvert, S. E., Pedersen, T. F. 1993. Geochemistry of Recent oxic and anoxic marine sediments: implications for the geological record. Marine Geology, Vol. 113, pp. 67-88.
  6. Cicioğlu, E. 1995. Sorgun (Yozgat) Kömürlerinin Kimyasal ve Petrografik Özelliklerinin İncelenmesi,Yüksek Lisans Tezi, Hacettepe Üniversitesi,
  7. ANKARA Chu, C. L., Chen, Q. L., Zhang, B., Shi, Z., Jiang, H. J., Yang, X. 2016. Influence on formation of Yuertusi Source Rock by hydrothermal activities at Dongergou section, Tarim Basin. Acta Sedimentol Sin., 34, Vol. 4, pp. 803–810.
  8. Cody, R. D. 1971. Adsorption and the reliability of trace elements as environmental indicators for shales. J. Sediment. Petrol., Vol. 41, pp. 461-471.
  9. Cox, R., Lowe, D. R., Cullers, R. L. 1995. The influence of sediment recycling and +” States. Geochim Cosmochim Acta, 59, Vol. 14, pp. 2919–2940.
  10. Crusius, J., Calvert, S., Pedersen, T., Sage, D. 1996. Rhenium and molybdenum enrichments in sediments as indicators of oxic, suboxic and sulfidic conditions of deposition. Earth Planet Science Letter, Amsterdam, Vol. 145, pp. 65–78.
  11. Dean, W. E. 1993. Physical properties, min