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Journal articles on the topic 'Feldspar Luminescence spectroscopy Luminescence dating'

Author: Grafiati

Published: 4 June 2021

Last updated: 12 February 2022

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1

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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2

Bringuier, Eric. "Disorder-enhanced luminescence kinetics in volcanic feldspars." EPJ Web of Conferences 244 (2020): 01012. http://dx.doi.org/10.1051/epjconf/202024401012.

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A granitic feldspar is well-ordered and has a stable thermoluminescence signal enabling its dating with high reliability. In contrast, a volcanic feldspar (sanidine) exhibits a slight cristallographic disorder and an anomalously fast fading of the thermoluminescence signal (Visocekas et al. 2014). It is shown here how disorder changes the decay of the signal and enhances the kinetics, while the increase in the microscopic complexity plays no role.

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3

Sohbati, Reza, Andrew Murray, Mayank Jain, et al. "Na-rich feldspar as a luminescence dosimeter in infrared stimulated luminescence (IRSL) dating." Radiation Measurements 51-52 (April 2013): 67–82. http://dx.doi.org/10.1016/j.radmeas.2012.12.011.

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4

Mueller, Daniela, Frank Preusser, Marius W. Buechi, Lukas Gegg, and Gaudenz Deplazes. "Luminescence properties and dating of glacial to periglacial sediments from northern Switzerland." Geochronology 2, no. 2 (2020): 305–23. http://dx.doi.org/10.5194/gchron-2-305-2020.

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Abstract. Luminescence dating has become a pillar of the understanding of Pleistocene glacial advances in the northern foreland of the Swiss Alps. However, both quartz and feldspar from the region are equally challenging as dosimeters with anomalous fading and partial bleaching being some of the obstacles to overcome for the establishment of decisive chronologies. In this study, luminescence properties of coarse- and fine-grained quartz, feldspar, and polymineral fractions of eight samples from a palaeovalley, Rinikerfeld in northern Switzerland, are systematically assessed. Standard performan

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5

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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6

Faershtein, Galina, Naomi Porat, and Ari Matmon. "Extended-range luminescence dating of quartz and alkali feldspar from aeolian sediments in the eastern Mediterranean." Geochronology 2, no. 1 (2020): 101–18. http://dx.doi.org/10.5194/gchron-2-101-2020.

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Abstract. Optically stimulated luminescence (OSL) of quartz is an established technique for dating late Pleistocene to late Holocene sediments. Unfortunately, this method is often limited to up to 100 ka (thousands of years). Recent developments in new extended-range luminescence techniques show great potential for dating older sediments of middle and even early Pleistocene age. These methods include thermally transferred OSL (TT-OSL) and violet stimulated luminescence (VSL) for quartz and post-infrared infrared stimulated luminescence (pIRIR) for feldspar. Here we investigate the luminescence

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7

Gong, Gelian, Bin Xia, and Shunsheng Liu. "Study on feldspar thermoluminescence spectra and its luminescence dating implication." Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms 251, no. 1 (2006): 143–47. http://dx.doi.org/10.1016/j.nimb.2006.05.022.

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8

Zhang, Junjie, and Sheng-Hua Li. "Review of the Post-IR IRSL Dating Protocols of K-Feldspar." Methods and Protocols 3, no. 1 (2020): 7. http://dx.doi.org/10.3390/mps3010007.

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Compared to quartz, the infrared stimulated luminescence (IRSL) of K-feldspar saturates at higher dose, which has great potential for extending the dating limit. However, dating applications with K-feldspar has been hampered due to anomalous fading of the IRSL signal. The post-IR IRSL (pIRIR) signal of K-feldspar stimulated at a higher temperature after a prior low-temperature IR stimulation has significantly lower fading rate. Different dating protocols have been proposed with the pIRIR signals and successful dating applications have been made. In this study, we review the development of vari

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9

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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10

Ollerhead, Jeff, D. J. Huntley, and Glenn W. Berger. "Luminescence dating of sediments from Buctouche Spit, New Brunswick." Canadian Journal of Earth Sciences 31, no. 3 (1994): 523–31. http://dx.doi.org/10.1139/e94-046.

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In this paper we describe our efforts to determine the formation chronology of a sequence of dunes on Buctouche Spit, a Holocene deposit on the northeast coast of New Brunswick. Optical dating, using infrared stimulation of K-feldspar grains, yielded ages ranging from 5 ± 30 a for an embryo dune to 765 ± 45 a for the oldest dune. Thermoluminescence ages, although less precise, support the recent formation of the dunes. The ages exhibit the expected sedation from youngest to oldest and are consistent with historical evidence coupled with an assumed constant sediment aggradation rate. The age re

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11

Madsen, Anni, Jan-Pieter Buylaert, and Andrew Murray. "Luminescence dating of young coastal deposits from New Zealand using feldspar." Geochronometria 38, no. 4 (2011): 379–90. http://dx.doi.org/10.2478/s13386-011-0042-5.

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Abstract A new measurement protocol has been tested on K-feldspars from Whanganui Inlet and Parengarenga Harbour, New Zealand. A Single Aliquot Regenerative (SAR) dose protocol, using two successive infrared (IR) stimulations (post-IR IR SAR protocol) is setup for these young (<1000 years) coastal sediments. Significant anomalous fading (g2days=7 %/decade) is observed using the conventional IR signal measured at 50°C. In contrast, the fading rate of the IR signal measured at elevated temperature (150°C) after the IR stimulation at 50°C (a post-IR IR signal) is not significant (g2days≤ 1 %/d

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12

Alappat, L., S. Tsukamoto, P. Singh, D. Srikanth, R. Ramesh, and M. Frechen. "Chronology of Cauvery Delta Sediments from Shallow Subsurface Cores Using Elevated-Temperature Post-IR IRSL Dating of Feldspar." Geochronometria 37, no. -1 (2010): 37–47. http://dx.doi.org/10.2478/v10003-010-0025-1.

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Chronology of Cauvery Delta Sediments from Shallow Subsurface Cores Using Elevated-Temperature Post-IR IRSL Dating of Feldspar We present the results of luminescence dating of sediments from two cores from the Cauvery Delta in south-east India. Since all natural quartz OSL signals except one sample were in saturation, the elevated temperature post-IR IRSL protocol for K-feldspar was applied to establish a chronology. Internal dose rates of K-feldspar grains were calculated from the measured internal content of potassium, uranium, thorium and rubidium in the bulk of K-feldspar grains using solu

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13

Lauer, Tobias, Rainer Bonn, Manfred Frechen, Magret Fuchs, Marcus Trier, and Sumiko Tsukamoto. "Geoarchaeological studies on Roman time harbour sediments in Cologne — comparison of different OSL dating techniques." Geochronometria 38, no. 4 (2011): 341–49. http://dx.doi.org/10.2478/s13386-011-0020-y.

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Abstract Due to the construction of a new North-South subway in Cologne, Roman time harbour sediments were exposed and were sampled for luminescence dating. A very good independent age control was given by the precise knowledge of the chronology of Roman activity and by radiocarbon ages of charcoal samples. Hence, different methodological approaches within luminescence dating were applied for Holocene heterogeneously bleached fluvial samples and were compared to the known ages. For one sample, optically stimulated luminescence (OSL) dating was applied to coarse-grained quartz using a single al

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14

Lamothe, Michel. "Dating the last 500 000 years of climate history using feldspar luminescence." Quaternary International 279-280 (November 2012): 263. http://dx.doi.org/10.1016/j.quaint.2012.08.654.

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15

Lamothe, Michel, Laurence Forget Brisson, and François Hardy. "Circumvention of anomalous fading in feldspar luminescence dating using Post-Isothermal IRSL." Quaternary Geochronology 57 (April 2020): 101062. http://dx.doi.org/10.1016/j.quageo.2020.101062.

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16

Stokes, Stephen, and Morteza Fattahi. "Red emission luminescence from quartz and feldspar for dating applications: an overview." Radiation Measurements 37, no. 4-5 (2003): 383–95. http://dx.doi.org/10.1016/s1350-4487(03)00060-x.

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17

Smedley, R. K., G. A. T. Duller, N. J. G. Pearce, and H. M. Roberts. "Determining the K-content of single-grains of feldspar for luminescence dating." Radiation Measurements 47, no. 9 (2012): 790–96. http://dx.doi.org/10.1016/j.radmeas.2012.01.014.

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18

Lauer, T., M. Krbetschek, B. Mauz, and M. Frechen. "Yellow stimulated luminescence from potassium feldspar: Observations on its suitability for dating." Radiation Measurements 47, no. 10 (2012): 974–80. http://dx.doi.org/10.1016/j.radmeas.2012.08.002.

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19

Buylaert, Jan-Pieter, Mayank Jain, Andrew S. Murray, Kristina J. Thomsen, Christine Thiel, and Reza Sohbati. "A robust feldspar luminescence dating method for Middle and Late Pleistocene sediments." Boreas 41, no. 3 (2012): 435–51. http://dx.doi.org/10.1111/j.1502-3885.2012.00248.x.

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20

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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21

Molodkov, Anatoly, Ivar Jaek, and Valery Vasilchenko. "Anomalous Fading of Ir-Stimulated Luminescence from Feldspar Minerals: Some Results of the Study." Geochronometria 26, no. -1 (2007): 11–17. http://dx.doi.org/10.2478/v10003-007-0007-0.

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Anomalous Fading of Ir-Stimulated Luminescence from Feldspar Minerals: Some Results of the StudyAn increasing amount of evidence shows that the use of feldspars in luminescence dating may suffer from significant age underestimates, which are thought to result from anomalous fading. In the hope of finding a solution to the problem we undertook physical investigations of kinetics and temperature dependencies of tunnel afterglow of these minerals. As a result, the method of the direct detection of the tunnel transitions from the dosimetric traps is proposed. Some other relevant results obtained a

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22

King, Georgina E., Sumiko Tsukamoto, Frédéric Herman, Rabiul H. Biswas, Shigeru Sueoka, and Takahiro Tagami. "Electron spin resonance (ESR) thermochronometry of the Hida range of the Japanese Alps: validation and future potential." Geochronology 2, no. 1 (2020): 1–15. http://dx.doi.org/10.5194/gchron-2-1-2020.

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Abstract. The electron spin resonance (ESR) of quartz has previously been shown to have potential for determining rock cooling histories; however, this technique remains underdeveloped. In this study, we explore the ESR of a suite of samples from the Hida range of the Japanese Alps. We develop measurement protocols and models to constrain the natural trapped-charge concentration as well as the parameters that govern signal growth and signal thermal decay. The thermal stability of the Al and Ti centres is similar to that of the luminescence of feldspar. Inverting the ESR data for cooling yields

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23

Gaar, Dorian, Sally Lowick, and Frank Preusser. "Performance of different luminescence approaches for the dating of known-age glaciofluvial deposits from northern Switzerland." Geochronometria 41, no. 1 (2014): 65–80. http://dx.doi.org/10.2478/s13386-013-0139-0.

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AbstractLuminescence properties of two samples taken from sand lenses in proglacial outwash de-posits of a piedmont glacier that reached the Swiss midlands during the Last Glacial Maximum are investigated in detail. Deconvolution of CW-OSL decay curves shows that the fast component dominates the OSL signal of quartz. The chemistry of single feldspar grains, in particular the K content in different grains, is determined using wavelength dispersive spectrometry (electron microprobe), revealing an average 12.9 wt.% K of the grains contributing to the IRSL signal. D e distributions are investigate

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24

Fattahi, Morteza, and Stephen Stokes. "Red luminescence from potassium feldspar for dating applications: a study of some properties relevant for dating." Radiation Measurements 37, no. 6 (2003): 647–60. http://dx.doi.org/10.1016/s1350-4487(03)00246-4.

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25

Barré, Magali, and Michel Lamothe. "Luminescence dating of archaeosediments: A comparison of K-feldspar and plagioclase IRSL ages." Quaternary Geochronology 5, no. 2-3 (2010): 324–28. http://dx.doi.org/10.1016/j.quageo.2009.03.004.

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26

Li, Bo, and Sheng-Hua Li. "Luminescence dating of K-feldspar from sediments: A protocol without anomalous fading correction." Quaternary Geochronology 6, no. 5 (2011): 468–79. http://dx.doi.org/10.1016/j.quageo.2011.05.001.

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27

Kars, Romée H., Tony Reimann, Christina Ankjaergaard, and Jakob Wallinga. "Bleaching of the post-IR IRSL signal: new insights for feldspar luminescence dating." Boreas 43, no. 4 (2014): 780–91. http://dx.doi.org/10.1111/bor.12082.

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28

Mittelstraß, Dirk, and Sebastian Kreutzer. "Spatially resolved infrared radiofluorescence: single-grain K-feldspar dating using CCD imaging." Geochronology 3, no. 1 (2021): 299–319. http://dx.doi.org/10.5194/gchron-3-299-2021.

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Abstract. The success of luminescence dating as a chronological tool in Quaternary science builds upon innovative methodological approaches, providing new insights into past landscapes. Infrared radiofluorescence (IR-RF) on K-feldspar is such an innovative method that was already introduced two decades ago. IR-RF promises considerable extended temporal range and a simple measurement protocol, with more dating applications being published recently. To date, all applications have used multi-grain measurements. Herein, we take the next step by enabling IR-RF measurements on a single grain level.

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29

Rades, Eike F., Sumiko Tsukamoto, Manfred Frechen, Qiang Xu, and Lin Ding. "A lake-level chronology based on feldspar luminescence dating of beach ridges at Tangra Yum Co (Southern Tibet)." Quaternary Research 83, no. 3 (2015): 469–78. http://dx.doi.org/10.1016/j.yqres.2015.03.002.

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Many lakes on the Tibetan Plateau exhibit strandplains with a series of beach ridges extending high above the current lake levels. These beach ridges mark former lake highstands and therefore dating their formation allows the reconstruction of lake-level histories and environmental changes. In this study, we establish a lake-level chronology of Tangra Yum Co (fifth largest lake on the Tibetan Plateau) based on luminescence dating of feldspar from 17 beach-ridge samples. The samples were collected from two strandplains southeast and north of the lake and range in elevation from the current shor

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ISHIBASHI, Toru, Issei SUZUKI, Haijiang LIU, Tomohiro TAKAGAWA, and Shinji SATO. "Development Process of Hamamatsu Strand Plain Elucidated from Optically Stimulated Luminescence Dating using Feldspar." Journal of Japan Society of Civil Engineers, Ser. B2 (Coastal Engineering) 65, no. 1 (2009): 611–15. http://dx.doi.org/10.2208/kaigan.65.611.

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31

Wallinga, J., A. S. Murray, G. A. T. Duller, and T. E. Törnqvist. "Testing optically stimulated luminescence dating of sand-sized quartz and feldspar from fluvial deposits." Earth and Planetary Science Letters 193, no. 3-4 (2001): 617–30. http://dx.doi.org/10.1016/s0012-821x(01)00526-x.

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32

Li, Bo, Sheng-Hua Li, Geoffrey A. T. Duller, and Ann G. Wintle. "Infrared stimulated luminescence measurements of single grains of K-rich feldspar for isochron dating." Quaternary Geochronology 6, no. 1 (2011): 71–81. http://dx.doi.org/10.1016/j.quageo.2010.02.003.

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33

Smedley, R. K., and N. J. G. Pearce. "Internal U, Th and Rb concentrations of alkali-feldspar grains: Implications for luminescence dating." Quaternary Geochronology 35 (October 2016): 16–25. http://dx.doi.org/10.1016/j.quageo.2016.05.002.

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34

Reimann, Tony, Christina Ankjærgaard, and Jakob Wallinga. "Testing the potential of a transferred IRSL (T-IRSL) feldspar signal for luminescence dating." Radiation Measurements 81 (October 2015): 275–81. http://dx.doi.org/10.1016/j.radmeas.2015.01.002.

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35

Al Khasawneh, Sahar, Andrew S. Murray, Stephen Bourke, and Dominik Bonatz. "Testing feldspar luminescence dating of young archaeological heated materials using potshards from Pella (Tell Tabqat Fahl) in the Jordan valley." Geochronometria 44, no. 1 (2017): 98–110. http://dx.doi.org/10.1515/geochr-2015-0056.

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Abstract Recent developments in the use of more stable feldspar signals in the luminescence dating of sediments offer the possibility of obtaining accurate feldspar luminescence ages for ceramic artefacts; this is especially interesting in locations which do not provide suitable quartz extracts. Here we examine the application of the stable infrared stimulated luminescence signal measured at elevated temperature (in this case 290°C; pIRIR290) after stimulation at about room temperature to Levantine pottery samples. A total of 52 potsherds were collected from three superimposed iron-age units a

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Li, Bo, Sheng-Hua Li, and Ann Wintle. "Overcoming Environmental Dose Rate Changes in Luminescence Dating of Waterlain Deposits." Geochronometria 30, no. -1 (2008): 33–40. http://dx.doi.org/10.2478/v10003-008-0003-z.

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Overcoming Environmental Dose Rate Changes in Luminescence Dating of Waterlain DepositsThis study investigates lacustrine and fluvial sediments on the Sala Us River in the Mu Us Desert in central north China. Significant changes in environmental dose rate in part of the section could be shown to have occurred from measurements of the present day radioactivity and by the age reversal for some samples that had been dated by optically stimulated luminescence (OSL) measurements on quartz. These changes in dose rate can be attributed to recent uptake of radioactive elements found in the sediments;

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37

Klasen, Nicole, Christa Loibl, Janet Rethemeyer, and Frank Lehmkuhl. "Testing feldspar and quartz luminescence dating of sandy loess sediments from the Doroshivtsy site (Ukraine) against radiocarbon dating." Quaternary International 432 (March 2017): 13–19. http://dx.doi.org/10.1016/j.quaint.2015.05.036.

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38

Jaek, I., A. Molodkov, and V. Vasilchenko. "Instability of luminescence responses in feldspar-and quartz-based paleo-dosimeters." Journal of Applied Spectroscopy 75, no. 6 (2008): 820–25. http://dx.doi.org/10.1007/s10812-009-9127-9.

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al Khasawneh, Sahar, Andrew Murray, Zeidan Kafafi, and Lucas Petit. "Luminescence Dating of the Iron Age Deposits from Tell Damiyah in the Jordan Valley." Radiocarbon 62, no. 1 (2019): 1–12. http://dx.doi.org/10.1017/rdc.2019.90.

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ABSTRACTIn this study, we investigate quartz-based luminescence optical dating of Iron Age deposits at the archaeological site of Tell Damiyah in the Jordan valley. Ten samples, taken from different occupation layers from two different excavation areas, proved to have good luminescence characteristics (fast-component dominated, dose recovery ratio 1.032 ± 0.010, n=24). The optical ages are completely consistent with both available 14C ages and ages based on stylistic elements; it appears that this material was fully reset at deposition, although it is recognised that the agreement with age con

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Thiel, Christine, Sumiko Tsukamoto, Kayoko Tokuyasu, et al. "Testing the application of quartz and feldspar luminescence dating to MIS 5 Japanese marine deposits." Quaternary Geochronology 29 (August 2015): 16–29. http://dx.doi.org/10.1016/j.quageo.2015.05.008.

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41

Tsukamoto, Sumiko, Reisuke Kondo, Tobias Lauer, and Mayank Jain. "Pulsed IRSL: A stable and fast bleaching luminescence signal from feldspar for dating Quaternary sediments." Quaternary Geochronology 41 (August 2017): 26–36. http://dx.doi.org/10.1016/j.quageo.2017.05.004.

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42

BUYLAERT, JAN-PIETER, SÉBASTIEN HUOT, ANDREW S. MURRAY, and PETER VAN DEN HAUTE. "Infrared stimulated luminescence dating of an Eemian (MIS 5e) site in Denmark using K-feldspar." Boreas 40, no. 1 (2010): 46–56. http://dx.doi.org/10.1111/j.1502-3885.2010.00156.x.

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43

Sohbati, Reza, Andrew Murray, Mayank Jain, Jan-Pieter Buylaert, and Kristina Thomsen. "Investigating the resetting of OSL signals in rock surfaces." Geochronometria 38, no. 3 (2011): 249–58. http://dx.doi.org/10.2478/s13386-011-0029-2.

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Abstract There are many examples of buried rock surfaces whose age is of interest to geologists and archaeologists. Luminescence dating is a potential method which can be applied to dating such surfaces; as part of a research project which aims to develop such an approach, the degree of resetting of OSL signals in grains and slices from five different cobbles/boulders collected from a modern beach is investigated. All the rock surfaces are presumed to have been exposed to daylight for a prolonged period of time (weeks to years). Feldspar was identified as the preferred dosimeter because quartz

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Thamó-Bozsó, Edit, Gábor Csillag, Judit Füri, Attila Nagy, and Árpád Magyari. "Age of sediments on Danube terraces of the pest plain (Hungary) based on optically stimulated luminescence dating of quartz and feldspar." Geochronometria 47, no. 1 (2020): 171–86. http://dx.doi.org/10.2478/geochr-2020-0021.

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Abstract The numerical ages available for the sediments on the Danube terraces in the Pest Plain are scarce. In this study, we present quartz OSL and K feldspar post-IR IRSL290 ages for the sandy fluvial, aeolian and slope sediments collected from Danube terraces IIb, III and V. The feldspar post-IR IRSL290 ages without residual dose subtraction are older than the quartz OSL ages, except for one sample, but the two sets of ages are overlapping within one or two sigma errors. In the bleaching experiment under natural sunlight during summer, an unbleachable component ranging from 2.5±0.7 Gy to 5

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Tamura, Toru, Kazumi Ito, Takahiko Inoue, and Tetsuya Sakai. "Luminescence dating of Holocene beach-ridge sands on the Yumigahama Peninsula, western Japan." Geochronometria 44, no. 1 (2017): 331–40. http://dx.doi.org/10.1515/geochr-2015-0076.

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Abstract We applied infrared stimulated luminescence (IRSL50) and post-infrared (post-IR) IRSL150 dating to K-feldspar sand obtained from Holocene beach ridges on the Yumigahama Peninsula, Japan, to investigate the rate of progradation of the beach, which has been affected by 17–18th century iron mining in a local river catchment. All samples showed higher equivalent doses for the post-IR IRSL signal. Fading tests indicated that IRSL yielded relatively high g-values (11–13%/decade), while post-IR IRSL yielded negative g-values (–5 to –8%/decade). The corrected IRSL age of the oldest sample, 8.

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Morthekai, P., Mayank Jain, Pedro Cunha, José Azevedo, and Ashok Singhvi. "An attempt to correct for the fading in million year old basaltic rocks." Geochronometria 38, no. 3 (2011): 223–30. http://dx.doi.org/10.2478/s13386-011-0033-6.

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Abstract The use of feldspar for luminescence dating has been restricted because of anomalous fading. This has made its application to several important geological problems such as volcanic terrains difficult. Presently, two correction procedures are used to correct for anomalous fading. The present study tests these correction procedures using volcanic samples of known ages spanning the time period of 400 ka to 2.2 Ma. These correction procedures provided grossly underestimated ages (up to 60%). The possible causes for the underestimation are discussed.

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King, Georgina. "Depositional pathway tracing in glacial catchments using Optically Stimulated Luminescence dating of K-feldspar and quartz." Quaternary International 279-280 (November 2012): 245–46. http://dx.doi.org/10.1016/j.quaint.2012.08.575.

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Li, Bo, and Sheng-Hua Li. "Luminescence dating of Chinese loess beyond 130 ka using the non-fading signal from K-feldspar." Quaternary Geochronology 10 (July 2012): 24–31. http://dx.doi.org/10.1016/j.quageo.2011.12.005.

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Li, Bo, Richard G. Roberts, Zenobia Jacobs, Sheng-Hua Li, and Yu-Jie Guo. "Construction of a ‘global standardised growth curve’ (gSGC) for infrared stimulated luminescence dating of K-feldspar." Quaternary Geochronology 27 (April 2015): 119–30. http://dx.doi.org/10.1016/j.quageo.2015.02.010.

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Lamothe, M., and M. Auclair. "The fadia method: a new approach in luminescence dating using the analysis of single feldspar grains." Radiation Measurements 32, no. 5-6 (2000): 433–38. http://dx.doi.org/10.1016/s1350-4487(00)00124-4.

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