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Relevant bibliographies by topics / Thermoluminescence (TL) dating

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Academic literature on the topic 'Thermoluminescence (TL) dating'

Author: Grafiati

Published: 4 June 2021

Last updated: 12 February 2022

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Journal articles on the topic "Thermoluminescence (TL) dating"

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Murthy, K. V. R. "Thermoluminescence and its Applications: A Review." Defect and Diffusion Forum 347 (December 2013): 35–73. http://dx.doi.org/10.4028/www.scientific.net/ddf.347.35.

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The present review article contains various applications of Thermoluminescence. The phenomena of thermoluminescence (TL) or thermally stimulated luminescence (TSL) and optically stimulated luminescence (OSL) are widely used for measurement of radiation doses from ionizing radiations, viz. x-rays, γ rays and β particles. The applications of TL are initiated in the field of Geology followed by Archaeology, personal dosimetry, material characterization and many more to name. The TL technique has been found to be useful in dating specimens of geologically recent origin where all other conventional

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Lees, Brian G., Lu Yanchou, and John Head. "Reconnaissance Thermoluminescence Dating of Northern Australian Coastal Dune Systems." Quaternary Research 34, no. 2 (1990): 169–85. http://dx.doi.org/10.1016/0033-5894(90)90029-k.

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AbstractQuaternary lithostratigraphic units in coastal dunes have been dated at three locations in northern Australia, Cobourg Peninsula, Shelburne Bay, and Cape Flattery, by both radiocarbon dating of shell and organic carbon and thermoluminescence (TL) sediment dating. Both coarse fraction and fine fraction TL methods were used. Seventeen TL dates were measured. None of the TL dates contradict the ages given by radiocarbon. Where multiple TL dates were taken from a unit, they overlap within 2 standard deviation giving added confidence in the results. A phase of dune emplacement during the la

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Kusiak, Jarosław, Mariusz Rychter, and Marta Stasiak-Cyran. "Attempts at thermoluminescence dating of fired materials from the Przeworsk Culture settlements." Geochronometria 38, no. 4 (2011): 359–68. http://dx.doi.org/10.2478/s13386-011-0026-5.

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AbstractThe thermoluminescence (TL) dating method has a significant measurement error margin reaching almost 10%. Due to this fact it could be considered as little effective in case of such sites from the Roman period as burial grounds with many artefacts useful for archaeological dating. However, for many settlements from this period, where pottery is the only kind of artefacts, the TL method can give notable results. The main purpose of the study was to make an attempt at TL dating of pottery and clay daub samples from the Nieszawa Kolonia and Kręcieszki sites and to compare the obtained dat

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Rendell, H. M., M. R. Khanlary, P. D. Townsend, T. Calderon, and B. J. Luff. "Thermoluminescence spectra of minerals." Mineralogical Magazine 57, no. 387 (1993): 217–22. http://dx.doi.org/10.1180/minmag.1993.057.387.03.

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AbstractThermoluminescence (TL) studies of insulators, including crystals of minerals such as calcite, quartz or zircon, have resulted in the development of a wider range of applications in the fields of radiation dosimetry and archaeological and geological dating. Most conventional TL measurements are made by recording light emission during heating by means of broad-band optical filters and blue-sensitive photomultiplier tubes. Much more information may be gained by monitoring the details of the emission spectrum during thermoluminescence. TL spectra of minerals exhibit changes as a result of

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Lamothe, Michel, and David J. Huntley. "Thermoluminescence Dating of Late Pleistocene Sediments, St. Lawrence Lowland, Québec." Géographie physique et Quaternaire 42, no. 1 (2007): 33–44. http://dx.doi.org/10.7202/032707ar.

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ABSTRACT This paper presents the results of a thermoluminescence (TL) dating program applied to waterlaid sediments of Late Pleistocene age, collected in the central St. Lawrence Lowland, in eastern Canada. The apparent TL ages were obtained using a partial bleach method (R-Gamma) in which the TL from light-sensitive traps is separated from the total TL. Fluvial (modern), marine (late-glacial) lacustrine (interstadial) and glacio-lacustrine (stadial) sediments yielded apparent ages ranging from 4 to 135 ka, and in general, these ages agreed with available stratigraphic evidence. Whilst testing

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Łanczont, Maria, Andrij Bogucki, Jarosław Kusiak, and Oleksandr Sytnyk. "The results of thermoluminescence dating in the Halych IIC (Ukraine) profile as the expression of the conditions of mineral material deposition." Geochronometria 40, no. 1 (2013): 42–50. http://dx.doi.org/10.2478/s13386-012-0022-4.

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AbstractMany studies conducted in the last few years in Poland indicate that the results of thermoluminescence dating of loess are reliable and correspond well to their geological ages. They can form the basis for determination of the chronology of changes of palaeoenvironmental conditions. In this paper we report dating results from the Halych IIC profile (Halych Prydnistrov’ja region, Ukraine). Thermoluminescence dating of this profile gives new information about the influence of local conditions on the results of TL analysis. As much as 75% of the obtained results are distinctly overestimat

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Berger, G. W., J. J. Clague, and D. J. Huntley. "Thermoluminescence dating applied to glaciolacustrine sediments from central British Columbia." Canadian Journal of Earth Sciences 24, no. 3 (1987): 425–34. http://dx.doi.org/10.1139/e87-044.

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Glaciolacustrine and lacustrine sediments are important indicators of deglacial, interglacial, and nonglacial intervals within the Quaternary of Canada, yet there are no techniques for measuring their absolute deposition ages beyond the last ~ 50 000 years. In an attempt to develop an absolute dating tool for such sediments, we applied the partial bleach thermoluminescence (TL) dating technique to glaciolacustrine sediments of known age from central British Columbia. Samples were selected to represent both ice-proximal and ice-distal deposition and different modes of sedimentation.The results

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García-Haro, A. R., R. Bernal, C. Cruz-Vázquez, S. E. Burruel-Ibarra, V. R. Orante-Barrón, and F. Brown. "Study of the Thermoluminescent Characteristics of Ceramic Roof Tiles Exposed to Beta Radiation." MRS Proceedings 1481 (2012): 89–95. http://dx.doi.org/10.1557/opl.2012.1636.

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ABSTRACTIn this work, thermoluminescence (TL) characteristics of roof tile ceramic samples previously exposed to beta radiation are reported for the very first time. TL measurements were carried out using powdered samples obtained by the the fine-grained method, with grain size ranged from 300 nm to 5 μm. Characteristic thermoluminescence glow curves showed a complex structure with a dosimetric maximum located at ~ 200 °C. TL response of roof tile samples increases as the radiation dose increases in the 25 Gy to 1.6 kGy range. One response showed a linear behaviour, with no evidence of saturat

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Berger, Glenn W., and Don J. Easterbrook. "Thermoluminescence dating tests for lacustrine, glaciomarine, and floodplain sediments from western Washington and British Columbia." Canadian Journal of Earth Sciences 30, no. 9 (1993): 1815–28. http://dx.doi.org/10.1139/e93-160.

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To help further develop reliable procedures for accurate thermoluminescence (TL) dating of Quaternary waterlaid sediments, we tested TL dating procedures on sediment types rarely examined: six glaciolacustrine samples, three samples of glaciomarine drift, and eight samples of floodplain deposits. We used the partial-bleach (R-beta/gamma) technique applied to fine-silt polymineral grains. Results from our younger known-age glaciolacustrine sediments confirm earlier observations that only the clayey laminae are generally suitable for TL dating. A clayey lamina older than ca. 140 – 150 ka produce

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Ekdal, Elçin, Arzu Ege, Turgay Karali, and Zafer Derin. "Luminescence dating studies of Yeşilova Hoyuk." Geochronometria 39, no. 4 (2012): 268–75. http://dx.doi.org/10.2478/s13386-012-0013-5.

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Abstract Ceramic findings collected from Yeşilova Hoyuk located in Izmir were dated using the thermoluminescence dating technique. The area is of significant archaeological importance since it is the first prehistoric settlement in Izmir. Recent archeological observations suggest that human occupation of the region took place about 8500 years ago comparing to previously determined dates of 5000 years. Three samples collected from the same archaeological layer (Neolithic period) in Yeşilova Hoyuk were dated using the thermoluminescence method. Archaeological doses (AD) were obtained by single a

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Dissertations / Theses on the topic "Thermoluminescence (TL) dating"

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Templer, R. H. "Thermoluminescence techniques for dating zircon inclusions." Thesis, University of Oxford, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.376953.

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Parks, D. A. "TL dating and geochemistry of brickearths in S.E. England." Thesis, University of Sussex, 1989. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.282705.

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奥野, 充., Mitsuru Okuno, Ma Hanah T. Mirabueno та ін. "フィリピン共和国,ルソン島の火山活動に関する熱ルミネッセンス法と放射性炭素法による年代学的研究(第19回名古屋大学年代測定総合研究センターシンポジウム平成18(2006)年度報告,第2部)". 名古屋大学年代測定資料研究センター, 2007. http://hdl.handle.net/2237/13705.

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第19回名古屋大学年代測定総合研究センターシンポジウム平成18(2006)年度報告<第2部> Proceedings of the 19th symposiumon on Chronological Studies at the Nagoya University Center for Chronological Research in 2006 日時:平成19 (2007)年1月15日(月)～17日(水) 会場:名古屋大学シンポジオン Date:January15th-17th, 2007 Venue:Nagoya Uhiversity Symposion Hall

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"Fabrication of a thermoluminescence (TL) dating system and studies on some (TL) characteristics and the pre-dose dating method." Chinese University of Hong Kong, 1988. http://library.cuhk.edu.hk/record=b5885909.

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by Kwok Si Ho.<br>Chinese title in romanization: Re shi guang duan dai xi tong zhi zhi zao ji re shi guang zhi yi xie te xing you jian ji liang duan dai fa zhi yan jiu.<br>Thesis (M.Ph.)--Chinese University of Hong Kong, 1988.<br>Bibliography: leaves 98-101.

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"Investigation of some critical properties of thermoluminescence (TL) and TL dating of ancient Chinese pottery." Chinese University of Hong Kong, 1990. http://library.cuhk.edu.hk/record=b5886565.

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by Ng Man Fai.<br>Title also in Chinese.<br>Thesis (M.Phil.)--Chinese University of Hong Kong, 1990.<br>Bibliography: leaves 165-170.<br>Acknowledgement --- p.i<br>Abstract --- p.ii<br>Content --- p.iv<br>Chapter Chapter 1. --- Introduction<br>Chapter 1.1 --- Starting point --- p.1<br>Chapter 1.2 --- TL dating --- p.2<br>Chapter Chapter 2. --- Introduction to the unified model<br>Chapter 2.1 --- Introduction --- p.5<br>Chapter 2.2 --- The model itself --- p.5<br>Chapter Chapter 3. --- Experimental apparatus<br>Chapter 3.1 --- Thermoluminescence (TL) glow curve taking system --- p.10<br

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Book chapters on the topic "Thermoluminescence (TL) dating"

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"LUMINESCENCE DATING." In Questions and Answers on Thermoluminescence (TL) and Optically Stimulated Luminescence (OSL). WORLD SCIENTIFIC, 2008. http://dx.doi.org/10.1142/9789812818843_0005.

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