Dose Determination of Fluvial Sediments in Manisa

Year 2023, , 381 - 388, 29.12.2023

Müjde Durukan Gültepe Arzu Ege

https://doi.org/10.18466/cbayarfbe.1381567

Abstract

Quartz, which is one of the most abundant minerals in nature, can be found in magmatic and metamorphic forms, as well as the usual components of granite and sedimentary formations. Quartz minerals, which are also known as the main component of quartzites, are also known as gangue minerals in many mineralizations. Quartz samples from two different sampling levels, namely the Kaletepe lower and the Kaletepe upper region, used in the study were prepared. Thermoluminescence (TL) glow curves of the samples exposed to radiation with a 90Sr/90Y β source were recorded with a TLD reader. While peaks were obtained at approximately 270 °C from the glow curves of the Kaletepe lower samples irradiated with β source, peaks were obtained at approximately 270 °C and 350 °C from the Kaletepe upper samples. When the annual average dose and age values of the lower and upper Kaletepe samples are examined, it can be said that it was formed in a time period of ~8000 years between two areas with a height difference of 130m.

Keywords

Equivalent Dose, Fluvial Sediments, Thermoluminescence dating, Quartz.

Supporting Institution

This research is supported by grants from the Scientific and Technological Research Council of Turkey (TÜBİTAK) Contract No. TBAG 104T139, and the Ege University Science and Technology Research Center (EBİLTEM Contract No. 2007/BIL/020).

Project Number

(TÜBİTAK) Contract No. TBAG 104T139, EBİLTEM Contract No. 2007/BIL/020

References

• [1]. Stokes, S. (1999). Luminescence dating applications in geomorphological research. Enviromental Science,Geomorphology, vol. 29, 153-171.
• [2]. Shannon, M. A., Rittenour, T. M., Nelson, M.S., Ataee, N., Brown, N., DeWitt, R., Durcan, J., Evans, M., Feathers, J., Frouin, M., Guérin, G., Heydari, M., Huot, S., Jain, M., Keen-Zebert, A., Li, B., López, G. I., Neudorf, C., Porat, N., Rodrigues, K., Sawakuchi, A. O., Spencer J. Q. G. K (2022). Thomsen; Guide for interpreting and reporting luminescence dating results, GSA Bulletin, 135 (5-6): 1480–1502.
• [3]. Satılmış, U. S., Ege, A. (2019). Thermoluminescence response of UV irradiated cerium doped Sr3Y2(BO3)4 phosphor, Journal of the Institute of Science and Technology, 9(1): 169-176.
• [4]. McKeever, S.W.S. (1985). Thermoluminescence of solids. Cambridge University Press.
• [5]. McKeever, S.W.S., Moscovitch, M., Townsend, P. D. (1995). Thermoluminescence dosimetry materials: properties and uses. Nuclear Technology Publishing.
• [6]. Vij, D. R. (1998). Luminescence of Solids. Plenum Press, New York.
• [7]. Souza, D. N., de Lima, J.F., Valerio,M.E.G., Fantini, C., Pimenta, M.A., Moreira, R.L., Caldas, L.V.C. (2002). Influence of thermal treatment on the Raman, İnfrared and TL responses of natural topaz, Nuclear Inst. And Methods in Physics B, 230-235.
• [8]. Hashimoto, T., Yasuda, K., Sato, K., Sakaue, H., Katayama, H. (1998). Radiation-induced luminescence images and TL-property changes with thermal annealing treatment on Japanese twin quartz. Radiation Measurements, vol. 29, Issue 5,493-502.
• [9]. Huntley, D.J., Godfrey-Smith, D.I., Thewalt, M.L.W., Berger, G.W. (1988) Thermoluminescence spectra of some mineral samples relevant to thermoluminescence dating. Journal of Luminescence, vol. 39, Issue 3,123-136.
• [10]. Wintle, A.G., Murray, (2006). A. S. A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols, Radiation Measurements, 41: 369-391.
• [11]. Wintle, A. G. (2008). Luminescence dating: where it has been and where it is going. Boreas, 37: 471-482.
• [12]. Wintle, A.G., Adamiec, G. (2017). Optically stimulated signals from quartz: A review, Radiation Measurements, vol. 98, 10-33pp.
• [13]. Capaldi, T. N., Rittenour, T. M., Nelson, M. S. (2022). Downstream changes in quartz OSL sensitivity in modern river sand reflects sediment source variability: Case studies from Rocky Mountain and Andean rivers, Quaternary Geochronology, vol. 71, 101317.
• [14]. Gray, H. J., Jain, M., Sawakuchi, A. O., Mahan, S. A., Tucker, G. E. (2019). Luminescence as a sediment tracer and provenance tool, Reviews of Geophysics, 57, 987– 1017pp.
• [15]. Pacompia, Y., Supo-Ramos, J. G., Gonzales-Lorenzo, C. D., Callo-Escobar, D. J., Rocca, R. R., Pastrana, E. C., Gomes, M. B., Silva-Carrera, B. N., Watanabe, S., Ayca-Gallegos, O., Ayala-Arenas, J.S. (2023). Luminescence dating and firing temperature determination of ancient ceramics fragments from the Tunata-hill site in the Churajon archaeological complex in Arequipa, Peru, Radiation Physics and Chemistry, vol. 204, 110725.
• [16]. Al-Khasawneh, S. (2023). Optically Stimulated Luminescence Dating (OSL): Procedures and Applications to Archaeology Research in Jordan, Cultural Heritage: At the Intersection of the Humanities and the Sciences,357.
• [17]. Sözbilir, H. (2002). Geometry and origin of folding in the neogenesediments of the Gediz Graben, Western Anatolia, Turkey, Geodinamica Acta, 15: 277-288pp.
• [18]. Bozkurt, E., Sözbilir, H. (2004). Tectonic evolution of the Gediz graben: field evidence for an episodic, two-stage extension in western Turkey, Geological Magazine, 141, 63–79.
• [19]. Bozkurt, E., Sözbilir, H. (2006). Evolution of the large-scale active Manisa fault, southwest Turkey: implications on fault development and regional tectonics, Geodinamica Acta,19, 427-453.
• [20]. Zhu, L., Mitchell B. J., Akyol N., Cemen, I., Kekovalı K. (2006). Crustal thickness variations in the Aegean region and implications for the extension of continental crust, J. Geophys. Res.,111, B01301.
• [21]. Ege, A., Ekdal, E., Karali, T., Can, N. (2009). Annual dose measurement for luminescence dating in Salihli, Turkey. Turkish J. Eng. Env. Sci., 33, 21- 29.
• [22]. Ege A., (2008). Dating Geological Samples Using Radiation Techniques, Ege University, Graduate School of Natural and Applied Sciences, Department of Nuclear Sciences, (PhD Thesis), İzmir.