Relevant bibliographies by topics / TT-OSL

Academic literature on the topic 'TT-OSL'

Author: Grafiati
Published: 10 December 2022
Last updated: 28 January 2023

Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles

Select a source type:

Contents

Consult the lists of relevant articles, books, theses, conference reports, and other scholarly sources on the topic 'TT-OSL.'

Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.

You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.

Journal articles on the topic "TT-OSL"

1

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 (May 7, 2020): 101–18. http://dx.doi.org/10.5194/gchron-2-101-2020.

Full text
Abstract:
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 behaviour of the TT-OSL, VSL, and pIRIR signals of quartz and feldspar minerals of aeolian sediments of Nilotic origin from the eastern Mediterranean. We sampled a 15 m thick sequence (Kerem Shalom) comprising sandy calcic palaeosols, which is part of a sand sheet that covers an extensive region in south-western Israel. Dose recovery and bleaching experiments under natural conditions indicated that the pIRIR250 signal is the most suitable for dating the Nilotic feldspar. Luminescence intensity profiles revealed natural saturation of the three signals at the same depth of ∼6 m, indicating that ages of samples below that depth are minimum ages. Using TT-OSL and pIRIR250, a minimum age of 715 ka for the base of the section was obtained, suggesting aeolian sand accumulation along the eastern Mediterranean coastal plain already since the early Pleistocene. Our results indicate that both TT-OSL and pIRIR250 can accurately date aeolian sediments of Nilotic origin up to 200 ka and that minimum ages can be provided for older samples up to the early Pleistocene.
APA, Harvard, Vancouver, ISO, and other styles
2

Porat, N., G. A. T. Duller, H. M. Roberts, and A. G. Wintle. "A simplified SAR protocol for TT-OSL." Radiation Measurements 44, no. 5-6 (May 2009): 538–42. http://dx.doi.org/10.1016/j.radmeas.2008.12.004.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Chapot, M. S., H. M. Roberts, G. A. T. Duller, and Z. P. Lai. "Natural and laboratory TT-OSL dose response curves: Testing the lifetime of the TT-OSL signal in nature." Radiation Measurements 85 (February 2016): 41–50. http://dx.doi.org/10.1016/j.radmeas.2015.11.008.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Hernandez, Marion, Barbara Mauz, Norbert Mercier, and Zhixiong Shen. "Evaluating the efficiency of TT-OSL SAR protocols." Radiation Measurements 47, no. 9 (September 2012): 669–73. http://dx.doi.org/10.1016/j.radmeas.2012.04.017.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Arnold, Lee J., Martina Demuro, Nigel A. Spooner, Gavin J. Prideaux, Matthew C. McDowell, Aaron B. Camens, Elizabeth H. Reed, et al. "Single-grain TT-OSL bleaching characteristics: Insights from modern analogues and OSL dating comparisons." Quaternary Geochronology 49 (February 2019): 45–51. http://dx.doi.org/10.1016/j.quageo.2018.01.004.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Faershtein, G., N. Porat, and A. Matmon. "Natural saturation of OSL and TT-OSL signals of quartz grains from Nilotic origin." Quaternary Geochronology 49 (February 2019): 146–52. http://dx.doi.org/10.1016/j.quageo.2018.04.002.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Faershtein, Galina, Benny Guralnik, Renske Lambert, Ari Matmon, and Naomi Porat. "Investigating the thermal stability of TT-OSL main source trap." Radiation Measurements 119 (December 2018): 102–11. http://dx.doi.org/10.1016/j.radmeas.2018.09.010.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

Adamiec, G., G. A. T. Duller, H. M. Roberts, and A. G. Wintle. "Improving the TT-OSL SAR protocol through source trap characterisation." Radiation Measurements 45, no. 7 (August 2010): 768–77. http://dx.doi.org/10.1016/j.radmeas.2010.03.009.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

Pagonis, V., A. G. Wintle, R. Chen, and X. L. Wang. "A theoretical model for a new dating protocol for quartz based on thermally transferred OSL (TT-OSL)." Radiation Measurements 43, no. 2-6 (February 2008): 704–8. http://dx.doi.org/10.1016/j.radmeas.2008.01.025.

Full text
APA, Harvard, Vancouver, ISO, and other styles
10

Zander, A., and A. Hilgers. "Testing the potential of OSL, TT-OSL, IRSL and post-IR IRSL luminescence dating on a Middle Pleistocene sediment record of Lake El'gygytgyn, Russia." Climate of the Past Discussions 8, no. 5 (September 28, 2012): 4779–815. http://dx.doi.org/10.5194/cpd-8-4779-2012.

Full text
Abstract:
Abstract. Lake El'gygytgyn is a 12 km wide crater lake located in remote Chukotka in the far East Russian Arctic about 100 km to the north of the Arctic Circle. It was formed by a meteorite impact about 3.58 Ma ago. This study tests the paleomagnetic and proxy data-based Mid- to Late-Pleistocene sediment deposition history using novel luminescence dating techniques of sediment cores taken from the centre of the 175 m deep lake. For dating polymineral and quartz fine grains (4–11 μm grain size range) were extracted from nine different levels from the upper 28 m of sediment cores 5011-1A and 5011-1B. Polymineral sub-samples were analysed by infra-red stimulated luminescence (IRSL) and post-IR infra-red stimulated luminescence (post-IR IRSL) using single aliquot regenerative dose (SAR) sequences. SAR protocols were further applied to measure the blue light optically stimulated luminescence (OSL) and thermally-transferred OSL (TT-OSL) of fine-grained quartz supplemented by a multiple aliquot TT-OSL approach. According to an independent age model, the lowest sample from 27.8–27.9 m below lake bottom level correlates to the Brunhes-Matuyama (B/M) reversal. Finally, the SAR post-IR-IRSL protocol applied to polymineral fine grains was the only luminescence technique able to provide dating results of acceptable accuracy up to ca. 700 ka. Major factors limiting precision and accuracy of the luminescence chronology are, for some samples, natural signals already approaching saturation level, and overall the uncertainty related to the sediment water content and its variations over geological times.
APA, Harvard, Vancouver, ISO, and other styles
More sources

Dissertations / Theses on the topic "TT-OSL"

1

Moffatt, Jillian Elizabeth. "Testing the TT-OSL single-aliquot protocol for quartz sediment dating." Thesis, 2014. http://hdl.handle.net/2440/85972.

Full text
Abstract:
Thermally-transferred optically stimulated luminescence (TT-OSL) is a form of optically stimulated luminescence that saturates at much higher doses than conventional OSL (Wang et al, 2006b). Luminescence sediment dating is a technique whereby the natural radiation dose given to a sample is measured. This is divided by the environmental radiation rate of the sample site to give the sample's age. As TT-OSL is able to measure higher doses than conventional OSL, it has been considered a candidate for long range luminescence sediment dating, beyond one million years. In this thesis, TT-OSL single-aliquot sediment dating protocols were tested on selected samples from the south-east of South Australia (SESA) stranded dune sequence, a sequence of ancient dunes ranging from 0 to 900 thousand years of age that have previously been independently dated using luminescence and non-luminescence dating methods. A young sample with a high natural dose from Baldina Creek, Burra, South Australia was also dated. Measurements of the thermal depletion of the TT-OSL signal were also made. It was found that, for the SESA samples, TT-OSL dating results do not agree with previous independent measurements above 200 ka. The results for the young Baldina Creek sample were within the expected range.
Thesis (M.Phil.) -- University of Adelaide, School of Chemistry and Physics, 2014
APA, Harvard, Vancouver, ISO, and other styles

Conference papers on the topic "TT-OSL"

1

Tew-Todd, Victoria, Steven L. Forman, Connor Mayhack, Liliana Marin, Logan Wiest, and Griffin Money. "EOLIAN DEPOSITIONAL AND ENVIRONMENTAL HISTORY FOR THE MONAHANS DUNE SYSTEM, WEST TEXAS FOR THE PAST CA. 0.5 MA BY THERMAL-TRANSFER OPTICALLY STIMULATED LUMINESCENCE (TT-OSL) DATING." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-354752.

Full text
APA, Harvard, Vancouver, ISO, and other styles
You might also be interested in the extended bibliographies on the topic 'TT-OSL' for particular source types:
Journal articles
We offer discounts on all premium plans for authors whose works are included in thematic literature selections. Contact us to get a unique promo code!

To the bibliography