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Artykuły w czasopismach na temat „Luminescence dating”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 25 lipca 2025

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1

Moska, Piotr, Andrzej Bluszcz, Grzegorz Poręba, et al. "Luminescence Dating Procedures at the Gliwice Luminescence Dating Laboratory." Geochronometria 48, no. 1 (2021): 1–15. http://dx.doi.org/10.2478/geochr-2021-0001.

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Abstract The Gliwice Luminescence Laboratory (GLL) is a part of the Institute of Physics – Centre for Science and Education at the Silesian University of Technology, which has gradually evolved since the 1980s. To date, nearly 3500 samples have been dated using luminescence from materials such as ceramics, bricks, and sediments from archaeological and geological sites. Currently, the laboratory is equipped with four luminescence readers and three gamma spectrometers, allowing luminescence dating of approximately 300 samples annually for the needs of research projects. This article focuses on t

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2

Chauhan, N. "Luminescence Dating: Basic Approach to Geochronology." Defect and Diffusion Forum 347 (December 2013): 111–37. http://dx.doi.org/10.4028/www.scientific.net/ddf.347.111.

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Nowadays, luminescence dating technique has become one of the unique tools for paleoclimatic studies. A lot of progress has been made in terms of understanding the phenomenon of luminescence, development of methodology for luminescence dating and its application. Still there are several directions which require better understanding and refinement. This brief review article focuses on the different aspects of luminescence dating, covering basic theory behind luminescence and luminescence dating, procedural aspects, complications and issues of luminescence dating and future perspective.

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Schmidt, Christoph, Théo Halter, Paul R. Hanson, et al. "Zircon luminescence dating revisited." Geochronology 6, no. 4 (2024): 665–82. https://doi.org/10.5194/gchron-6-665-2024.

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Abstract. Luminescence dating plays a pivotal role in Quaternary science, yet ongoing methodological challenges persist in refining the temporal range, accuracy, and precision of luminescence methods. Our contribution revisits zircons as potential alternative dosimeters to quartz, feldspar, or calcite for routine dating applications. The essential advantage of zircons over other minerals is the time-invariant and high internal dose rate due to high radionuclide contents, dominating over the external contribution, which is more challenging to assess. Reported drawbacks are low zircon abundance,

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4

Sharma, S. K. "Luminescence dating of Gyspum." Quaternary International 279-280 (November 2012): 444. http://dx.doi.org/10.1016/j.quaint.2012.08.1456.

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Lang, Andreas, Uwe Rieser, Jan Habermann, and Günther A. Wagner. "Luminescence Dating of Sediments." Science of Nature 85, no. 11 (1998): 515–23. http://dx.doi.org/10.1007/s001140050543.

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Andričević, P., E. L. Sellwood, T. Freiesleben, et al. "Dating fractures using luminescence." Earth and Planetary Science Letters 624 (December 2023): 118461. http://dx.doi.org/10.1016/j.epsl.2023.118461.

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7

Rhodes, Ed. "Holocene book review: Luminescence dating: guidelines on using luminescence dating in archaeology." Holocene 19, no. 4 (2009): 680–81. http://dx.doi.org/10.1177/09596836090190041303.

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8

Wintle, A. "Future Directions of Luminescence Dating of Quartz." Geochronometria 37, no. -1 (2010): 1–7. http://dx.doi.org/10.2478/v10003-010-0023-3.

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Future Directions of Luminescence Dating of Quartz Recent developments in our understanding of the limitations of optically stimulated luminescence as a dating tool are presented alongside summaries of results obtained on other luminescence signals measured in sedimentary quartz grains.

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9

Jain, Mayank, and Lars Bøtter-Jensen. "Luminescence Instrumentation." Defect and Diffusion Forum 357 (July 2014): 245–60. http://dx.doi.org/10.4028/www.scientific.net/ddf.357.245.

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This chapter gives an introduction to instrumentation for stimulated luminescence studies, with special focus on luminescence dating using the natural dosimeters, quartz and feldspars. The chapter covers basic concepts in luminescence detection, and thermal and optical stimulation, and reference irradiation. It then briefly describes development of spectrometers in dating applications, and finally gives an overview of recent development in the field directly linked to novel instrumentation. Contents of Paper

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10

Peng, Jun, ZhiBao Dong, Feng Qing Han, Hao Long, and Xiang Jun Liu. "R package numOSL: numeric routines for optically stimulated luminescence dating." Ancient TL 31, no. 2 (2013): 41–48. https://doi.org/10.26034/la.atl.2013.473.

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In luminescence dating, there are various software packages that can be used to do data analysis, such as Analyst, Java RadialPlotter, SigmaplotTM and so on. There is also an open source R package Luminescence, which has the capacity to tackle not only lots of basic statistical analysis but also provide more advanced data treatment. In this article, we present another R package, numOSL, the aim of which is neither to present a comprehensive numeric tool for luminescence dating just as the R package Luminescence did, nor to cover all numeric topics regarding luminescence dating. We focus only o

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11

Zhao, Hua, Zhe Liu, Cheng-Min Wang, and Sheng-Hua Li. "Luminescence dating of volcanic eruptions in Datong, northern China." Quaternary Geochronology 30 (October 2015): 357–62. http://dx.doi.org/10.1016/j.quageo.2015.04.012.

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Rogge, Corina E., and Julie Arslanoglu. "Luminescence of coprecipitated titanium white pigments: Implications for dating modern art." Science Advances 5, no. 5 (2019): eaav0679. http://dx.doi.org/10.1126/sciadv.aav0679.

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Material analysis of cultural artifacts can uncover aspects of the creative process and help determine the origin and authenticity of works of art. Technical studies on abstract expressionist paintings revealed a luminescence signature from titanium white paints whose pigments were manufactured by coprecipitation with calcium or barium sulfate. We propose that trace neodymium present in some ilmenite (FeTiO3) ores can be trapped in the alkaline earth sulfate during coprecipitation, generating a luminescent marker characteristic of the ore and process. We show that the luminescence is linked to

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13

Cordier, S., M. Frechen, and S. Tsukamoto. "Methodological Aspects on Luminescence Dating of Fluvial Sands from the Moselle Basin, Luxembourg." Geochronometria 35, no. -1 (2010): 67–74. http://dx.doi.org/10.2478/v10003-010-0006-4.

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Methodological Aspects on Luminescence Dating of Fluvial Sands from the Moselle Basin, LuxembourgOptically stimulated luminescence (OSL) dating of quartz and infrared-stimulated luminescence (IRSL) dating of feldspar were applied to fluvial sands from the lower terrace (M1) of the Moselle valley in Luxembourg (western Europe). The dating results indicated that the aggradation period for the sediments from below the M1 alluvial terrace can be correlated to the Weichselian upper Pleniglacial (MIS 2), which is in good agreement with the general chronostratigraphy of the Moselle terrace staircase.

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14

Wallinga, J., F. Davids, and J. W. A. Dijkmans. "Luminescence dating of Netherlands’ sediments." Netherlands Journal of Geosciences 86, no. 3 (2007): 179–96. http://dx.doi.org/10.1017/s0016774600077799.

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AbstractOver the last decades luminescence dating techniques have been developed that allow earth scientists to determine the time of deposition of sediments. In this contribution we review: 1) the development of the methodology; 2) tests of the reliability of luminescence dating on Netherlands’ sediments; and 3) geological applications of the method in the Netherlands. Our review shows that optically stimulated luminescence dating of quartz grains using the single aliquot regenerative dose method yields results in agreement with independent age control for deposits ranging in age from a few y

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15

Li, Guo-Qiang, Hui Zhao, and Fa-Hu Chen. "Comparison of three K-feldspar luminescence dating methods for Holocene samples." Geochronometria 38, no. 1 (2011): 14–22. http://dx.doi.org/10.2478/s13386-011-0011-z.

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Abstract The luminescence dating of the K-feldspar fraction is an alternative way for samples that cannot yield reasonable equivalent dose (De) from quartz fraction with very weak luminescence signal. For testing the reliability of the infrared stimulated luminescence (IRSL) dating of K-feldspar, luminescence dating was applied to quartz and K-feldspar fractions respectively for several Holocene samples in this study. K-feldspar apparent ages using routine single aliquot regenerative-dose (SAR) protocol, K-feldspar ages using g value correction method and ages from isochron dating method were

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16

Duller, G. A. T. "Recent developments in luminescence dating of Quaternary sediments." Progress in Physical Geography: Earth and Environment 20, no. 2 (1996): 127–45. http://dx.doi.org/10.1177/030913339602000201.

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Luminescence dating is an important technique for providing chronological control for Quaternary sedimentary sequences. In this article recent developments in luminescence dating are described, together with the implications of these developments for the application of the various types of luminescence dating techniques now available. In particular, the development of optically stimulated luminescence (OSL) techniques has had a profound effect upon the field, enabling younger materials to be dated, increasing the diversity of depositional environments that can be dated, and allowing the develo

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17

Stella, Giuseppe, Dorotea Fontana, Anna Gueli, and Sebastiano Troja. "Different approaches to date bricks from historical buildings." Geochronometria 41, no. 3 (2014): 256–64. http://dx.doi.org/10.2478/s13386-013-0157-y.

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Abstract The application of Thermally (TL) and Optically (OSL) Stimulated Luminescence on bricks used as building material has allowed solving an chronological issue in the field of historical building dating. The possibility to use one or more methodologies of dating is closely related to the luminescent and granulometric characteristics of the sample. Using some brick samples collected in the church of Sain Seurin in Bordeaux (France), this paper discusses the implications and the possibility to use different approaches and techniques for dating. With this aim luminescence measurements were

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18

Preusser, Frank, Detlev Degering, Markus Fuchs, et al. "Luminescence dating: basics, methods and applications." E&G Quaternary Science Journal 57, no. 1/2 (2008): 95–149. http://dx.doi.org/10.3285/eg.57.1-2.5.

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Abstract. Luminescence dating is a tool frequently used for age determination of Quaternary materials such as archaeological artefacts, volcanic deposits and a variety of sediments from different environmental settings. The present paper gives an overview of the physical basics of luminescence dating, the necessary procedures from sampling to age calculation, potential problems that may interfere with correct age calculation as well as procedures to identify and resolve those problems. Finally, a brief summary of the most common fields of application is given ranging from artefacts to the vari

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19

Munyikwa, K., M. Telfer, I. Baker, and C. Knight. "Core drilling of Quaternary sediments for luminescence dating using the Dormer Drillmite." Ancient TL 29, no. 1 (2011): 16–21. https://doi.org/10.26034/la.atl.2011.445.

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The coring of buried Quaternary deposits using a Dormer DrillmiteTM auger permits the extraction of samples for luminescence dating from depths of up to 20 m. The unit is powered hydraulically and features portability as one of its main advantages. While a range of other power drilling methods have been used successfully for sample collection in a number of luminescence dating studies, there is a dearth of literature that describes such drilling methods in detail. The absence of such information belies the importance of sampling methods in luminescence dating. This contribution aims to play a

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20

Singh, Priyanka, S N Ali, Kuldeep Prakash, and P Morthekai. "Efficacy of fading correction procedures to date Late Quaternary Higher Central Himalayan lacustrine sediment." Journal of Scientific Research 67, no. 04 (2023): 06–11. http://dx.doi.org/10.37398/jsr.2023.670402.

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Feldspar luminescence dating method has a wider dynamic dating range than quartz due to its larger sensitivity and higher luminescence saturation level. However, feldspar luminescence fades ‘anomalously’ with time that generally underestimates the age using feldspar. To correct the anomalous fading of the luminescence signal, three procedures have been devised. We examined the efficacy of fading correction procedures on lacustrine sediment samples from the Central Himalayan region. We observed that two correction procedures (HL and LM) are insufficiently corrective, but HK works well.

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21

Panzeri, L., A. Galli, F. Maspero, M. Saleh, and M. Martini. "The activities of the LAMBDA (Laboratory of Milano Bicocca university for Dating and Archaeometry): what’s new?" Journal of Physics: Conference Series 2204, no. 1 (2022): 012047. http://dx.doi.org/10.1088/1742-6596/2204/1/012047.

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Abstract The LAMBDA, Laboratory of Milano Bicocca University for Dating and Archaeometry, has a forty-years experience started with the first thermoluminescence dating activities in Italy in the early eighties. Soon after, other dating techniques (Optically Stimulated Luminescence, OSL, Radiocarbon, Dendrochronology and recently Rehydroxylation) have been studied and dedicated laboratories have been set up, where the physical basis of the techniques are constantly under investigation, mainly for what concerns the role of defects in quartz in the luminescence processes. LAMBDA covers other prom

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22

Tamura, Toru. "Optically Stimulated Luminescence (OSL) Dating." RADIOISOTOPES 70, no. 3 (2021): 107–16. http://dx.doi.org/10.3769/radioisotopes.70.107.

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23

Antrobus, Abby. "Luminescence Dating of Brick Chimneys." Vernacular Architecture 35, no. 1 (2004): 21–31. http://dx.doi.org/10.1179/vea.2004.35.1.21.

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24

Rendell, H. M. "Luminescence dating of Quaternary sediments." Geological Society, London, Special Publications 89, no. 1 (1995): 223–35. http://dx.doi.org/10.1144/gsl.sp.1995.089.01.11.

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Clarke, Michèle L., Helen M. Rendell, and Ann G. Wintle. "Quality assurance in luminescence dating." Geomorphology 29, no. 1-2 (1999): 173–85. http://dx.doi.org/10.1016/s0169-555x(99)00013-6.

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Wintle, Ann. "Dating Sediments Using Luminescence Signals." Environmental Science & Technology 27, no. 5 (1993): 803–5. http://dx.doi.org/10.1021/es00042a600.

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Kook, M. H., A. S. Murray, T. Lapp, et al. "A portable luminescence dating instrument." Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms 269, no. 12 (2011): 1370–78. http://dx.doi.org/10.1016/j.nimb.2011.03.014.

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Feathers, James K., Maria Nieves Zedeño, Lawrence C. Todd, and Stephen Aaberg. "Dating Stone Alignments by Luminescence." Advances in Archaeological Practice 3, no. 4 (2015): 378–96. http://dx.doi.org/10.7183/2326-3768.3.4.378.

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AbstractStone alignments, including tipi rings and drive lines, are abundant on the northern Plains and adjacent Rocky Mountains, but they have been notoriously difficult to date. This paper applies luminescence dating to sediments directly underneath the rocks to estimate the age of placement of the rock. This is based on the assumption that before the rock was emplaced, turbation processes brought sufficient grains to the surface, where sunlight reset the signal. Single-grain dating of potassium feldspars allowed isolation of these original well-bleached grains, which by now have built up a

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29

Burbidge, Christopher Ian. "Facets of Luminescence for Dating." Spectroscopy Letters 45, no. 2 (2012): 118–26. http://dx.doi.org/10.1080/00387010.2011.610657.

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WINTLE, A. G. "FIFTY YEARS OF LUMINESCENCE DATING." Archaeometry 50, no. 2 (2008): 276–312. http://dx.doi.org/10.1111/j.1475-4754.2008.00392.x.

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Prescott, J. R., and G. B. Robertson. "Luminescence dating: an Australian perspective." Australian Journal of Earth Sciences 55, no. 6-7 (2008): 997–1007. http://dx.doi.org/10.1080/08120090802097468.

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Lian, Olav B., and Richard G. Roberts. "Dating the Quaternary: progress in luminescence dating of sediments." Quaternary Science Reviews 25, no. 19-20 (2006): 2449–68. http://dx.doi.org/10.1016/j.quascirev.2005.11.013.

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Liritzis, Ioannis. "Surface dating by luminescence: An overview." Geochronometria 38, no. 3 (2011): 292–302. http://dx.doi.org/10.2478/s13386-011-0032-7.

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AbstractDaylight radiation resets luminescence ‘clock’ to zero on rock surfaces, but transmission depends on the transparency of the rock. On burial, surfaces are no longer exposed to daylight and accumulation of trapped electrons takes place till the excavation. This reduction of luminescence as a function of depth fulfils the prerequisite criterion of daylight bleaching. Thus rock artefacts and monuments follow similar bleaching rationale as those for sediments. In limestone and marble, daylight can reach depths of 0.5–1 mm and up to 16 mm respectively, while for other igneous rocks e.g. qua

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Kreutzer, S., C. Burow, M. Dietze, M. C. Fuchs, M. Fischer, and C. Schmidt. "Software in the context of luminescence dating: status, concepts and suggestions exemplified by the R package ‘Luminescence’." Ancient TL 35, no. 2 (2017): 1–11. https://doi.org/10.26034/la.atl.2017.513.

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The relevance of luminescence dating is reflected by the steadily growing quantity of published data. At the same time, the amount of data available for analysis has increased due to technological and methodological advances. Routinely, luminescence data are analysed using a mixture of commercially available software, self-written tools and specific solutions. Based on a luminescence dating literature screening we show how rarely articles report on the software used for the data analysis and we discuss potential problems arising from this. We explore the growing importance of the statistical p

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Kreutzer, Sebastian, Christoph Schmidt, Margret C. Fuchs, Michael Dietze, Manfred Fischer, and Markus Fuchs. "Introducing an R package for luminescence dating analysis." Ancient TL 30, no. 1 (2012): 1–8. https://doi.org/10.26034/la.atl.2012.457.

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For routine luminescence dating applications the commonly used Risø readers are bundled with analysis software, such as Viewer or Analyst. These software solutions are appropriate for most of the regular dating and publication jobs, and enable assessment of luminescence characteristics and provide basic statistical data treatment. However, for further statistical analysis and data treatments, this software may reach its limits. In such cases, open programming languages are a more appropriate approach. Here, we present the R package ‘Luminescence’ for a more flexible handling of luminescence da

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Nelson, Michelle S., Harrison J. Gray, Jack A. Johnson, Tammy M. Rittenour, James K. Feathers, and Shannon A. Mahan. "User Guide for Luminescence Sampling in Archaeological and Geological Contexts." Advances in Archaeological Practice 3, no. 2 (2015): 166–77. http://dx.doi.org/10.7183/2326-3768.3.2.166.

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AbstractLuminescence dating provides a direct age estimate of the time of last exposure of quartz or feldspar minerals to light or heat and has been successfully applied to deposits, rock surfaces, and fired materials in a number of archaeological and geological settings. Sampling strategies are diverse and can be customized depending on local circumstances, although all sediment samples need to include a light-safe sample and material for dose-rate determination. The accuracy and precision of luminescence dating results are directly related to the type and quality of the material sampled and

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Frechen, Manfred, Erzsébet Horváth, and Gyula Gábris. "Geochronology of Middle and Upper Pleistocene Loess Sections in Hungary." Quaternary Research 48, no. 3 (1997): 291–312. http://dx.doi.org/10.1006/qres.1997.1929.

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The application of both thermoluminescence and infrared stimulated luminescence dating to the extensively studied “classical” Hungarian loess/paleosol sequences from Basaharc, Mende, and Paks provides a reliable chronological framework and climatostratigraphic reconstruction for the last interglacial/glacial cycle. Based on this combined luminescence dating study a new chronology is proposed for the “Young Loess” in Hungary. Luminescence dating suggests that the loess below the MF2 horizon formed during the penultimate glaciation. The MF1 horizon probably formed during an interstade within oxy

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Biswas, R. H. "Development and Application of Luminescence to Earth and Planetary Sciences: Some Landmarks." Defect and Diffusion Forum 357 (July 2014): 217–43. http://dx.doi.org/10.4028/www.scientific.net/ddf.357.217.

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Luminescence, mainly thermoluminescence (TL) and optically stimulated luminescence (OSL), has been researched for more than five decades towards its application to earth and planetary sciences. Luminescence production mechanism has been understood through several theoretical studies, like analytical kinetic theory, numerical models along with the experimental results. Instrument development has progressed with aim from user friendly TL/OSL reader dedicated for dating to challenging reader forin-situMartian sediment dating. Since the development of optical dating in 1985, the technique revoluti

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Li, Bo, Zenobia Jacobs, Richard Roberts, and Sheng-Hua Li. "Review and assessment of the potential of post-IR IRSL dating methods to circumvent the problem of anomalous fading in feldspar luminescence." Geochronometria 41, no. 3 (2014): 178–201. http://dx.doi.org/10.2478/s13386-013-0160-3.

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AbstractQuartz has been the main mineral used for optically stimulated luminescence (OSL) dating of sediments over the last decade. The quartz OSL signal, however, has been shown to saturate at relatively low doses of ∼200–400 Gy, making it difficult to be used for dating beyond about 200 thou-sand years (ka), unless the environmental dose rate is low. The infrared stimulated luminescence (IRSL) from feldspars has been shown to continue to grow to higher dose levels than quartz OSL. The application of IRSL dating of feldspars, however, has long been hampered by the anomalous fading effect. Rec

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Bouvier, Armel, Grégory Pinto, Pierre Guibert, David Nicolas-Méry, and Maylis Baylé. "Luminescence dating applied to medieval architecture." ArchéoSciences, no. 34 (April 10, 2010): 59–68. http://dx.doi.org/10.4000/archeosciences.2619.

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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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Feathers, James K. "Use of luminescence dating in archaeology." Measurement Science and Technology 14, no. 9 (2003): 1493–509. http://dx.doi.org/10.1088/0957-0233/14/9/302.

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Stokes, Stephen. "Luminescence dating applications in geomorphological research." Geomorphology 29, no. 1-2 (1999): 153–71. http://dx.doi.org/10.1016/s0169-555x(99)00012-4.

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Prescott, J. R., and G. B. Robertson. "Sediment dating by luminescence: a review." Radiation Measurements 27, no. 5-6 (1997): 893–922. http://dx.doi.org/10.1016/s1350-4487(97)00204-7.

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Wintle, Ann G. "Luminescence dating: laboratory procedures and protocols." Radiation Measurements 27, no. 5-6 (1997): 769–817. http://dx.doi.org/10.1016/s1350-4487(97)00220-5.

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Habermann, Jan, Thomas Schilles, Regina Kalchgruber, and Günther A. Wagner. "Steps towards surface dating using luminescence." Radiation Measurements 32, no. 5-6 (2000): 847–51. http://dx.doi.org/10.1016/s1350-4487(00)00066-4.

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