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Journal articles on the topic 'Luminescence dating'

Author: Grafiati

Published: 4 June 2021

Last updated: 26 July 2024

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1

Moska, Piotr, Andrzej Bluszcz, Grzegorz Poręba, Konrad Tudyka, Grzegorz Adamiec, Agnieszka Szymak, and Aleksandra Przybyła. "Luminescence Dating Procedures at the Gliwice Luminescence Dating Laboratory." Geochronometria 48, no. 1 (January 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 the laboratory procedures used in GLL to obtain luminescence ages. Recent improvements of the GLL's facilities and new equipment, as well as the performance spanning the Laboratory's 30 years of activity, are discussed in terms of obtained results and the involvement in national and international projects.

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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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3

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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4

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

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5

Andričević, P., E. L. Sellwood, T. Freiesleben, A. J. Hidy, M. Kook, M. C. Eppes, and M. Jain. "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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6

Rhodes, Ed. "Holocene book review: Luminescence dating: guidelines on using luminescence dating in archaeology." Holocene 19, no. 4 (May 20, 2009): 680–81. http://dx.doi.org/10.1177/09596836090190041303.

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7

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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8

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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9

Wintle, A. "Future Directions of Luminescence Dating of Quartz." Geochronometria 37, no. -1 (January 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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10

Rogge, Corina E., and Julie Arslanoglu. "Luminescence of coprecipitated titanium white pigments: Implications for dating modern art." Science Advances 5, no. 5 (May 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 a specific ilmenite source used in historic TITANOX pigments, is not present in pigments produced by more advanced chemistries, and provides dating information. Facile Raman-based detection of this luminescence, along with characteristic peaks of rutile, anatase, calcium sulfate, or barium sulfate, can identify the type of titanium white pigment and narrow its manufacture date range.

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11

Wallinga, J., F. Davids, and J. W. A. Dijkmans. "Luminescence dating of Netherlands’ sediments." Netherlands Journal of Geosciences 86, no. 3 (September 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 years up to 125 ka. Optical dating of quartz has successfully been applied to sediments from a wide range of depositional environments such as coastal dunes, cover sands, fluvial channel deposits, colluvial deposits and fimic soils. These results demonstrate that optical dating is a powerful tool to explore the natural archive of the Netherlands’ subsurface.

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12

Cordier, S., M. Frechen, and S. Tsukamoto. "Methodological Aspects on Luminescence Dating of Fluvial Sands from the Moselle Basin, Luxembourg." Geochronometria 35, no. -1 (January 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. The ages were obtained from small aliquots of quartz and feldspars, using the single aliquot regenerative (SAR) protocol. The equivalent dose determination included a series of tests and the selection of the Minimum Age Model as the most appropriate statistical model. This made it possible to provide a reliable methodological background for further luminescence dating of fluvial sediments from the Moselle basin.

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13

Li, Guo-Qiang, Hui Zhao, and Fa-Hu Chen. "Comparison of three K-feldspar luminescence dating methods for Holocene samples." Geochronometria 38, no. 1 (March 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 compared with quartz ages. It is found that the g value correction method cannot give reliable ages due to the large errors induced during measurements. The isochron dating method is effective to the sample with problematically external dose rate. However, isochron dating may introduce a relatively greater error during grain sizes — De curve fitting, therefore this method could obtain low-resolution ages for Holocene samples. Even K-feldspar apparent age from routine SAR protocol is relatively younger by about 10% than the quartz age, it still could establish reasonable chronological framework for Holocene samples.

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Stella, Giuseppe, Dorotea Fontana, Anna Gueli, and Sebastiano Troja. "Different approaches to date bricks from historical buildings." Geochronometria 41, no. 3 (September 1, 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 performed on both polymineral fine grain and quartz inclusion phases extracted from each brick. For Equivalent Dose (ED) and consequently age determination, TL on mixed fine grain fraction (FG), OSL on quartz inclusions (QI) and on mixed fine grain (FG*) fraction, were used. The results obtained suggest the advantage of using OSL technique on fine grain fraction cleaned up by IR stimulation (FG*), but the use of quartz inclusion represents indeed a good alternative.

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15

Duller, G. A. T. "Recent developments in luminescence dating of Quaternary sediments." Progress in Physical Geography: Earth and Environment 20, no. 2 (June 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 development of novel methods of age determination. The most exciting developments are the ability to obtain luminescence ages for samples in the age range from 100 to 1000 years, and the ability to date individual sand grains from a sample.

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16

Preusser, Frank, Detlev Degering, Markus Fuchs, Alexandra Hilgers, Annette Kadereit, Nicole Klasen, Matthias Krbetschek, Daniel Richter, and Joel Q. G. Spencer. "Luminescence dating: basics, methods and applications." E&G Quaternary Science Journal 57, no. 1/2 (August 1, 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 variety of different sediments suitable for luminescence dating.

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17

Tamura, Toru. "Optically Stimulated Luminescence (OSL) Dating." RADIOISOTOPES 70, no. 3 (March 15, 2021): 107–16. http://dx.doi.org/10.3769/radioisotopes.70.107.

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18

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

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19

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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20

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

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21

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

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22

Kook, M. H., A. S. Murray, T. Lapp, P. H. Denby, C. Ankjærgaard, K. Thomsen, M. Jain, J. H. Choi, and G. H. Kim. "A portable luminescence dating instrument." Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms 269, no. 12 (June 2011): 1370–78. http://dx.doi.org/10.1016/j.nimb.2011.03.014.

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23

Feathers, James K., Maria Nieves Zedeño, Lawrence C. Todd, and Stephen Aaberg. "Dating Stone Alignments by Luminescence." Advances in Archaeological Practice 3, no. 4 (November 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 signal because the rock prevents transfer to the surface. Plotting the number of original well-bleached grains with depth showed that these grains were concentrated just under the rock and decreased with depth. This is what would be predicted if the assumption is true. Dates were derived from several samples from Kutoyis in north central Montana, from Whitewater in eastern Montana, and from several sites in northwestern Wyoming. Many samples from Kutoyis and Wyoming dated to the last 600 years, but some samples from both places were more than 2,000 years old. The Whitewater features also dated to around 2,000 years ago. The ages are consistent with the cultural history of the areas.

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24

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

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25

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

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26

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

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27

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

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28

Liritzis, Ioannis. "Surface dating by luminescence: An overview." Geochronometria 38, no. 3 (September 1, 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. quartz in granites, partial bleaching occurs up to 5mm depth under several hours of daylight exposures and almost complete beaching is achieved in the first 1 mm within about 1 min daylight exposure. The ‘quartz technique’ for limestone monuments containing traces of quartz enables their dating with Optically Stimulated Luminescence (OSL) techniques. The surface luminescence (thermoluminescence, TL or OSL) dating has been developed and further refined on various aspects of equivalent dose determination, complex radiation geometry, incomplete bleaching etc. A historical review of the development including important applications, along with some methodological aspects are discussed.

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29

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 (April 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 prominent archaeometry fields such as dating of mortars by OSL and Radiocarbon, surface dating of bricks and rehydroxylation dating. In this paper we will present the recent results in dating field focusing on mortar and surface dating. Furthermore, the results of a recent dating campaign to rediscover ancient Milan will be presented.

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30

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 (May 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 sample collection methods in the field. Selection of target material for dating should include considerations of adequacy of resetting of the luminescence signal (optical and thermal bleaching), the ability to characterize the radioactive environment surrounding the sample (dose rate), and the lack of evidence for post-depositional mixing (bioturbation in soils and sediment). Sample strategies for collection of samples from sedimentary settings and fired materials are discussed. This paper should be used as a guide for luminescence sampling and is meant to provide essential background information on how to properly collect samples and on the types of materials suitable for luminescence dating.

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31

Frechen, Manfred, Erzsébet Horváth, and Gyula Gábris. "Geochronology of Middle and Upper Pleistocene Loess Sections in Hungary." Quaternary Research 48, no. 3 (November 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 oxygen isotope stage 3. For the youngest loess, overlying MF1, a very high accumulation rate was determined. Large time gaps occur above MF2 and MF1, indicating that most of the record of the last glaciation is missing in the standard sections at Basaharc, Mende, and Paks. Either large discontinuities or a very low accumulation rate occurred in all three type sections during the soil-forming periods. High-resolution studies of climatic proxies using this combined luminescence dating approach provide a reliable chronological framework for loess and loess derivatives of the last glacial cycle in Hungary, although a precise and complete chronostratigraphic reconstruction cannot be achieved from the incomplete records found at these sites.

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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 (December 1, 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 aliquot regenerative dose method (SAR) for thermoluminescence (TL) using coarse grain quartz minerals extracted from samples. Thick and thin Al2O3:C thermoluminescence dosimeters (TLD) were used to determine the annual dose rate. The archaeological doses were found to vary from 25.91±0.78 to 26.82±0.68 Gy, and the annual doses were found to be between 3.34±0.24 and 3.47±0.24 mGy/a. The ages obtained for the samples were determined to be 6000±830 BC, 5740±670 BC and 5460±740 years for samples ND1, ND2 and ND3, respectively, which supports the prediction of archeologist that the sampling layer dates from the Neolithic period.

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34

Feathers, James K. "Use of luminescence dating in archaeology." Measurement Science and Technology 14, no. 9 (July 29, 2003): 1493–509. http://dx.doi.org/10.1088/0957-0233/14/9/302.

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35

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

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36

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

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37

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

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38

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

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Barnett, S. M. "Sampling pottery in luminescence dating studies." Radiation Measurements 32, no. 5-6 (December 2000): 467–72. http://dx.doi.org/10.1016/s1350-4487(00)00099-8.

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40

Feathers, James K., and Elena Migliorini. "Luminescence dating at Katanda — a reassessment." Quaternary Science Reviews 20, no. 5-9 (December 2001): 961–66. http://dx.doi.org/10.1016/s0277-3791(00)00041-x.

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41

Wintle, A. G. "Infrared-stimulated luminescence dating of sediments." Radiation Measurements 23, no. 2-3 (April 1994): 607–12. http://dx.doi.org/10.1016/1350-4487(94)90107-4.

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42

WINTLE, ANN G. "Luminescence dating of Quaternary sediments - Introduction." Boreas 37, no. 4 (November 2008): 469–70. http://dx.doi.org/10.1111/j.1502-3885.2008.00060.x.

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43

LANG, A., and G. A. WAGNER. "INFRARED STIMULATED LUMINESCENCE DATING OF ARCHAEOSEDIMENTS." Archaeometry 38, no. 1 (February 1996): 129–41. http://dx.doi.org/10.1111/j.1475-4754.1996.tb00766.x.

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44

Liritzis, Ioannis, Vassilios Aravantinos, George S. Polymeris, Nikolaos Zacharias, Ioannis Fappas, George Agiamarniotis, Ioanna K. Sfampa, Asimina Vafiadou, and George Kitis. "Witnessing prehistoric Delphi by luminescence dating." Comptes Rendus Palevol 14, no. 3 (April 2015): 219–32. http://dx.doi.org/10.1016/j.crpv.2014.12.007.

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45

Feathers, James K. "Luminescence dating and modern human origins." Evolutionary Anthropology: Issues, News, and Reviews 5, no. 1 (1996): 25–36. http://dx.doi.org/10.1002/(sici)1520-6505(1996)5:1<25::aid-evan7>3.0.co;2-v.

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46

Lepper, Kenneth. "Optically stimulated luminescence dating an introduction." New Mexico Geology 29, no. 4 (2007): 111. http://dx.doi.org/10.58799/nmg-v29n4.111.

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47

Clarke, M. L., C. A. Richardson, and H. M. Rendell. "Luminescence dating of mojave desert sands." Quaternary Science Reviews 14, no. 7-8 (January 1995): 783–89. http://dx.doi.org/10.1016/0277-3791(95)00051-8.

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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 revolutionised the research in earth sciences. And since then to recent, many methodologies have been developed and some are in developing stage using different signals, like, single grain OSL, red TL, time resolved OSL, thermally transferred OSL (TT-OSL), post infrared-infrared stimulated luminescence (pIR-IRSL), violet light stimulated luminescence (VSL), infrared radioluminescence (IRRL), etc. with an objective to improve the accuracy and precision and to extend the dating range. The wide range of application in different environment, e.g. aeolian, fluvial, marine, glacier, soil, volcanic materials, heated materials, shocked materials, meteorites, etc. have made the technique successful to understand the quaternary history of earth and planetary information like terrestrial and cosmic ray exposure ages of meteorite, meteoroid orbit, thermal metamorphism history of meteorite etc. The aim of this present paper is to discuss some landmarks and recent trends in the development and application in these areas. Contents of the Paper

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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 (September 1, 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. Recent progress in understanding anomalous fading of the infrared stimulated luminescence (IRSL) signals in potassium-feldspar has led to the development of post-IR IRSL (pIRIR) protocols and also a multiple elevated temperature (MET) stimulation (MET-pIRIR) protocol. These procedures have raised the prospect of isolating a non-fading IRSL component for dating Quaternary deposits containing feldspars. In this study, we review the recent progress made on (1) overcoming anomalous fading of feldspar, and (2) the development of pIRIR dating techniques for feldspar. The potential and problems associated with these methods are discussed.

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Lauer, Tobias, Manfred Frechen, and Peter Fischer. "Luminescence dating of the Lower Middle Terrace site at Brühl, southern Lower Rhine Embayment – a first dating approach." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 168, no. 1 (March 1, 2017): 105–14. http://dx.doi.org/10.1127/zdgg/2017/0109.

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