Relevant bibliographies by topics / Quartz; Thermoluminescence dating; Thermoluminescence

Academic literature on the topic 'Quartz; Thermoluminescence dating; Thermoluminescence'

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Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "Quartz; Thermoluminescence dating; Thermoluminescence"

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Huntley, D. J., D. I. Godfrey-Smith, M. L. W. Thewalt, J. R. Prescott, and J. T. Hutton. "Some quartz thermoluminescence spectra relevant to thermoluminescence dating." International Journal of Radiation Applications and Instrumentation. Part D. Nuclear Tracks and Radiation Measurements 14, no. 1-2 (January 1988): 27–33. http://dx.doi.org/10.1016/1359-0189(88)90038-6.

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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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SHEINKMAN, Vladimir S., Oleg A. SIMONOV, and Yuliya Yu ERINA. "NUMERICAL SIMULATION OF THERMOLUMINESCENCE QUARTZ PARTICLE." Tyumen State University Herald. Physical and Mathematical Modeling. Oil, Gas, Energy 7, no. 3 (2021): 136–51. http://dx.doi.org/10.21684/2411-7978-2021-7-3-136-151.

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One of the widely used methods for studying minerals is the thermoluminescent (TL) method, which is used to date Quaternary sedimentary rocks. Usually, the difficulty in using TL dating is the lack of information about the structure of the mineral used in the experiment. For reliable interpretation of experimental data, the authors applied the digital twin method. In this case, all stages of the transformation of the mineral used are modeled from its burial in sedimentary rocks to the stimulation of the TL-signal splash in it under laboratory conditions on special installations, taking into account the unevenness heat transfer inside the sample of this mineral. The paper presents the results of numerical simulation of the TL signal from a spherical particle of natural quartz. The modeling was carried out in two stages. At the first stage, the influence of the burial time of quartz in the sedimentary rocks on its TL signal was determined. For this, the problem was posed of the accumulation of the crystal lattice quartz, information about the time of its presence in the natural radiation field. At the second stage, the TL signal from a spherical particle was simulated, which was heated in an experimental setup from the surface according to a linear law. It was found that, firstly, the burial time of quartz affects the shape of the TL-curve and, therefore, the mineral is applicable for dating. Secondly, it is necessary to control the heating mode of the quartz sample, since at high heating rates, heat transfer irregularities are significant for particles with a large radius. It also affects the shape of the TL signal and, as a result, can make it difficult to obtain age definitions or distort them. To assess the effect of non-uniformity of heat transfer, a dimensionless similarity parameter was proposed, which connects the radius of the particles and the heating rate.
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Murthy, K. V. R. "Thermoluminescence and its Applications: A Review." Defect and Diffusion Forum 347 (December 2013): 35–73. http://dx.doi.org/10.4028/www.scientific.net/ddf.347.35.

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The present review article contains various applications of Thermoluminescence. The phenomena of thermoluminescence (TL) or thermally stimulated luminescence (TSL) and optically stimulated luminescence (OSL) are widely used for measurement of radiation doses from ionizing radiations, viz. x-rays, γ rays and β particles. The applications of TL are initiated in the field of Geology followed by Archaeology, personal dosimetry, material characterization and many more to name. The TL technique has been found to be useful in dating specimens of geologically recent origin where all other conventional methods fail. It has been found to be highly successful in dating ancient pottery samples. The TL/OSL dating is done from a quartz grain, which is collected from pottery or brick, by reading the TL-output. The main basis in the Thermoluminescence Dosimetry (TLD) is that TL output is directly proportional to the radiation dose received by the phosphor and hence provides the means of estimating the dose from unknown irradiations. The TL dosimeters are being used in personnel, environmental and medical dosimetry. During the last two decades, OSL based dosimeters have also been used for various applications. Natural and induced TL signals can be used to explore mineral, oil and natural gas. The present review presents TL theory, TL of minerals, salt, cement, salt crystals from pickles, and low temperature thermoluminescence (LLTL) of few agricultural products. Contents of Paper
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VALLADAS, H., and G. VALLADAS. "THERMOLUMINESCENCE DATING OF BURNT FLINT AND QUARTZ: COMPARATIVE RESULTS." Archaeometry 29, no. 2 (August 1987): 214–20. http://dx.doi.org/10.1111/j.1475-4754.1987.tb00414.x.

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Fedorowicz, Stanislaw, and Algirdas Gaigalas. "Geochronological and Sedimentological Interpretation of Interglacial Aquatic Sediments based on TL Dating." Geochronometria 35, no. -1 (January 1, 2010): 75–83. http://dx.doi.org/10.2478/v10003-010-0003-7.

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Geochronological and Sedimentological Interpretation of Interglacial Aquatic Sediments based on TL DatingFor the first time sedimentological interpretation of absolute ages obtained by thermoluminescence method on aquatic interglacial sediments was made. The analyzed size fractions of quartz grains were 160-250, 125-160, 100-125, 80-100 and 63-80 μm. The youngest and most reliable ages from 22 analyzed samples were obtained from the following quartz grain size granulometric fractions: 160-250 μm - 3 cases, 125-160 μm - 7, 100-125 μm - 6, 80-100 μm - 3 and 63-80 μm - 2 cases. Therefore, it may be concluded that the most suitable fractions for thermoluminescence dating are 125-160 μm and 100-125 μm. While evaluating the results of thermoluminescence dating it is necessary to take into account the procedure of sampling from layers of interest, their lithological composition, first of all granulometric, sedimentary environment, including sources of material, the material getting to the load flows, transportation mode and basin differentiation. From all the granulometric fractions of a sample, age of fine-grained fraction (63-80 μm) may be explained by the input of aeolian dust to a basin and sedimentation along with clasts brought to a lake by water flows. Aeolian sand storms performed precise multigenetic sedimentation that was active during that time. Bimodality of granulometric composition is defined by input of material from various sources of different composition. Older ages were obtained in the case of positive granulometric asymmetry. After sedimentological interpretation of thermoluminescence (TL) dating we can state that formation of aquatic fine-grained sands occurred 83.6±10 - 116.1±13 and 130.2±15 - 276.4±32 thousand years (ky) ago. Those geochronological zones coincide with interg lacial periods of Merkine (75.5-114 ky) and Snaigupele (180-280 ky) in Lithuania.
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Rendell, H. M., M. R. Khanlary, P. D. Townsend, T. Calderon, and B. J. Luff. "Thermoluminescence spectra of minerals." Mineralogical Magazine 57, no. 387 (June 1993): 217–22. http://dx.doi.org/10.1180/minmag.1993.057.387.03.

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AbstractThermoluminescence (TL) studies of insulators, including crystals of minerals such as calcite, quartz or zircon, have resulted in the development of a wider range of applications in the fields of radiation dosimetry and archaeological and geological dating. Most conventional TL measurements are made by recording light emission during heating by means of broad-band optical filters and blue-sensitive photomultiplier tubes. Much more information may be gained by monitoring the details of the emission spectrum during thermoluminescence. TL spectra of minerals exhibit changes as a result of crystal purity, radiation dose, dose rate and thermal history. This paper exemplifies the additional information available as a result of spectral studies, and focuses on investigations undertaken by the University of Sussex TL group. Examples include work on calcite, fluorite, zircon and feldspars.
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Miallier, D., J. Faïn, and S. Sanzelle. "Single-quartz-grain thermoluminescence dating: An approach for complex materials." Nuclear Tracks and Radiation Measurements (1982) 10, no. 1-2 (January 1985): 163–68. http://dx.doi.org/10.1016/0735-245x(85)90021-3.

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Haustein, M., and M. R. Krbetschek. "Red Thermoluminescence of Quartz and its Application in Dating Archaeometallurgical Slag." Radiation Protection Dosimetry 101, no. 1 (August 1, 2002): 375–78. http://dx.doi.org/10.1093/oxfordjournals.rpd.a006005.

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Kim, K. B., and D. G. Hong. "Analytical investigations of thermoluminescence glow curve on quartz for luminescence dating." Radiation Measurements 81 (October 2015): 232–36. http://dx.doi.org/10.1016/j.radmeas.2015.01.019.

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Dissertations / Theses on the topic "Quartz; Thermoluminescence dating; Thermoluminescence"

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韓志勇 and Zhiyong Han. "Thermoluminescence dating of granitic quartz." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 1999. http://hub.hku.hk/bib/B31238555.

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Han, Zhiyong. "Thermoluminescence dating of granitic quartz /." Hong Kong : University of Hong Kong, 1999. http://sunzi.lib.hku.hk/hkuto/record.jsp?B21583766.

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Chen, Yongye. "Study of luminescence signals from quartz and their applications in geothermometry." Click to view the E-thesis via HKUTO, 2008. http://sunzi.lib.hku.hk/hkuto/record/b40203955.

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Chen, Geng, and 陳耿. "Studies of quartz luminescence sensitivity relevant to dating and dosimetry." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2000. http://hub.hku.hk/bib/B42576143.

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Chen, Geng. "Studies of quartz luminescence sensitivity relevant to dating and dosimetry." Click to view the E-thesis via HKUTO, 2000. http://sunzi.lib.hku.hk/hkuto/record/B42576143.

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Chen, Yongye, and 陳永曄. "Study of luminescence signals from quartz and their applications in geothermometry." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2008. http://hub.hku.hk/bib/B40203955.

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Zhao, Hui, and 趙暉. "Studies of isochron luminescence dating with sand-sized grains." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2002. http://hub.hku.hk/bib/B42577329.

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Zhao, Hui. "Studies of isochron luminescence dating with sand-sized grains." Click to view the E-thesis via HKUTO, 2002. http://sunzi.lib.hku.hk/hkuto/record/B42577329.

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McFee, Christopher James. "The use of an imaging photon detector for luminescence dating." Thesis, University of Oxford, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.296940.

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Salmazo, Giovana Oliveira [UNESP]. "Caracterização das propriedades termoluminescentes de sedimentos da formação geológica Rio Claro." Universidade Estadual Paulista (UNESP), 2009. http://hdl.handle.net/11449/91988.

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Made available in DSpace on 2014-06-11T19:25:33Z (GMT). No. of bitstreams: 0 Previous issue date: 2009-10-21Bitstream added on 2014-06-13T20:53:36Z : No. of bitstreams: 1 salmazo_go_me_ilha.pdf: 1435780 bytes, checksum: 267d629a52fdf58b7156f4c83fc33587 (MD5)
Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
A formação geológica Rio Claro constitui um dos mais importantes registros sedimentares cenozóicos da Depressão Periférica Paulista. Apesar de essa formação geológica ser muito estudada, sua idade ainda encontra-se indeterminada. De modo a contribuir aos conhecimentos sobre a formação geológica Rio Claro, o trabalho objetivou um estudo geocronológico de seus sedimentos. Para isso, foram estudas cinco amostras sedimentares coletadas de pontos arbitrários da formação geológica, as quais foram denominadas de DSRC- 09, DSRC-10, DSRC-21, DSRC-22 e DSRC-23, e caracterizadas pela técnica da termoluminescência (TL). Grãos de quartzo de diâmetros entre 75 a 180 μm foram utilizados na caracterização. As amostras apresentaram sinal de termoluminescência natural entre 200 e 450 °C. Com exceção da amostra DSRC 22, todas as amostras apresentaram região de Plateau, que indica a região da curva de emissão que se manteve estável durante o período geológico a temperatura ambiente. A região de Plateau de DSRC-09, DSRC-10, DSRC 21 e DSRC-23 compreendeu o intervalo de temperatura de 320 a 380 °C. Pelo método Tm-Tstop se observou a presença de três picos constituindo a curva de emissão termoluminescente nessa região de temperatura. O nível residual da TL foi obtido após 80 horas de exposição dos grãos de quartzo à luz solar. Os sedimentos apresentaram não estar saturados, pois a intensidade do sinal TL aumentou em função de dose adicional artificial. Para a avaliação da idade dos sedimentos, o pico de 325 °C foi isolado e a energia de ativação foi calculada pelo método de crescimento inicial. As idades de deposição obtidas para as amostras DSRC-09, DSRC-10 e DSRC-21 foram respectivamente de 188.000 anos, 210.000 anos e 166.000 anos.
The geological formation Rio Claro constitutes one the most important sedimentary records of São Paulo Peripheral Depression. Although this geological formation is too much studied, its age yet is not determinate. To contribute to knowledge about Rio Claro geological formation, the work aimed a geocronological study of its sediments. For this, five sedimentary samples collected from arbitrary points were studied, which were called DSRC-09, DSRC-10, DSRC- 21, DSRC-22 and DSCR 23, and characterized by thermoluminescence technique. Grains of quartz with diameter between 75 and 180 μm were utilized to characterize it. The samples showed natural thermoluminescence signal between 200 and 450 °C. Except for the sample DSRC 22, all samples showed Plateau region, indicating that the region of glow curve remained stable during the geological time at environment temperature. Plateau region of DSRC-09, DSCR-10, DSRC-21 and DSRC-23 was defined by temperature range of 320 °C to 380°C. The method Tm-Tstop showed that the glow curves are composed by tree peaks in this temperature range. The residual TL was obtained after 80 hours of sunlight exposure. The sediments had not been saturated, because the TL signal intensity increased according to the artificial additional dose. For evaluation of the age sediments, the 325 °C peak was isolated and the activation energy was calculated by the method initial rise. The deposition ages for the samples DSRC-09, DSRC-10 and DSRC-21were respectively 188.000, 210.000 and 166.000 years.
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Books on the topic "Quartz; Thermoluminescence dating; Thermoluminescence"

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Thermoluminescence dating. London: Academic Press, 1985.

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Aitken, M. J. An introduction to optical dating: The dating of Quaternary sediments by the use of photon-stimulated luminescence. Oxford: Oxford University Press, 1998.

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La termoluminiscencia en el fechamiento de sitios arqueológicos. México, D.F: Instituto Nacional de Antropología e Historia, 1989.

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Huppertz, Hannelore. Thermolumineszenzdatierung: Eine methodologische Analyse aufgrund stratigraphisch gesicherter Befunde. Frankfurt am Main: P. Lang, 2000.

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Fathony, Muhammad. Dosimetric characteristic studies of phototransfer thermoluminescence in natural quartz. Birmingham: University of Birmingham, 1992.

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Kenkyūjo, Tezukayama Kōkogaku. Kōkogaku ni okeru netsu ruminesensu nendai sokutei. Nara-shi: Tezukayama Kōkogaku Kenkyūjo, 1992.

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Thermolumineszenzdatierung: Eine methodologische Analyse aufgrund stratigraphisch geicherter Befunde. Frankfurt am Main: P. Lang, 2000.

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Dijkmans, Jos W. A. Aspects of geomorphology and thermoluminescence dating of cold-climate eolian sands. Amsterdam: Koninklijk Nederlands Aardrijkskundig Genootschap, 1990.

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Questions and answers on thermoluminescence and optically stimulated luminescence. Hackensack, N.J: World Scientific, 2008.

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Millard, Hugh T. Thermoluminescence dating procedures in use at the U.S. Geological Survey, Denver, Colorado. [Reston, Va.]: U.S. Dept. of the Interior, U.S. Geological Survey, 1994.

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Book chapters on the topic "Quartz; Thermoluminescence dating; Thermoluminescence"

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Martini, Marco. "Quartz Defects, Optically Stimulated Luminescence and Thermoluminescence." In Encyclopedia of Scientific Dating Methods, 1–8. Dordrecht: Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-6326-5_68-6.

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Martini, Marco. "Quartz Defects, Optically Stimulated Luminescence and Thermoluminescence." In Encyclopedia of Scientific Dating Methods, 650–56. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-007-6304-3_68.

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Richter, Daniel. "Dating Small Heated Flint Artifacts: A New Thermoluminescence Technique." In Neanderthal Lifeways, Subsistence and Technology, 53–57. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-94-007-0415-2_6.

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Bluszcz, Andrzej. "Thermoluminescence Dating of Deposits from the Area of Bir Sahara East and Bir Tarfawi." In Egypt During the Last Interglacial, 224–26. Boston, MA: Springer US, 1993. http://dx.doi.org/10.1007/978-1-4615-2908-8_13.

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Hemphill-Haley, Mark A., Thomas L. Sawyer, Peter L. K. Knuepfer, Steven L. Forman, and Ivan G. Wong. "Timing of Faulting Events from Thermoluminescence Dating of Scarp-Related Deposits, Lemhi Fault, Southeastern Idaho." In AGU Reference Shelf, 541–48. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/rf004p0541.

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Kyparissi-Apostolika, Nina, and Sotiris K. Manolis. "Reconsideration of the Antiquity of the Middle Palaeolithic Footprints from Theopetra Cave (Thessaly, Greece)." In Reading Prehistoric Human Tracks, 169–82. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-60406-6_10.

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AbstractDuring the 1996 field season, four footprints were found in undisturbed deposits at the borders of squares Θ10-I10 at a depth of 3.5 m at the Theopetra Cave excavation site. The footprints lie adjacent to an ash horizon that has been dated to ca ~135 ka. Two footprints in the trail are complete and measure 150.4 mm and 138.96 mm in length. Based on modern European standards, these lengths would be consistent with young children aged between 2 and 4 years old and 90–100 cm in stature. The two complete footprints, which follow each other in the trail, appear both to have been left feet. The partial print, which immediately precedes the two complete prints in the series, also appears to have been by a left foot. This suggests that what initially seems to be a single trail is actually a composite of two or more trails of prints. This hypothesis is supported by the different characteristics of the two complete prints. One is consistent with a bare foot and clearly shows the impressions of the toes, ball, arch and heel. The other is characterized by a simpler contour and is more sharply defined and indicates that the individual was wearing some kind of foot covering. An important question is what kind of hominid made the footprints? These footprints may have been made by Neanderthals or early Homo sapiens, based on thermoluminescence dating results.
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Duller, Geoff. "Thermoluminescence Dating." In Encyclopedia of Physical Science and Technology, 699–704. Elsevier, 2003. http://dx.doi.org/10.1016/b0-12-227410-5/00775-4.

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Musílek, L., and M. Kubelík. "Thermoluminescence Dating." In Radiation in Art and Archeometry, 101–28. Elsevier, 2000. http://dx.doi.org/10.1016/b978-044450487-6/50052-3.

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"Thermoluminescence Dating." In Encyclopedic Dictionary of Archaeology, 1380. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-58292-0_200342.

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"Thermoluminescence dating." In Thermoluminescence of Solids, 253–92. Cambridge University Press, 1985. http://dx.doi.org/10.1017/cbo9780511564994.008.

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Conference papers on the topic "Quartz; Thermoluminescence dating; Thermoluminescence"

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MARTINI, MARCO, and EMANUELA SIBILIA. "THERMOLUMINESCENCE DATING AND CULTURAL HERITAGE." In Science for Cultural Heritage - Technological Innovation and Case Studies in Marine and Land Archaeology in the Adriatic Region and Inland - VII International Conference on Science, Arts and Culture. WORLD SCIENTIFIC, 2010. http://dx.doi.org/10.1142/9789814307079_0007.

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Smaali, M. "Thermoluminescence of swept and doped irradiated quartz crystals." In 10th International Conference on European Frequency and Time. IEE, 1996. http://dx.doi.org/10.1049/cp:19960034.

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Bahadur, H. "Thermoluminescence investigations in Ge-doped cultured quartz crystals." In 18th European Frequency and Time Forum (EFTF 2004). IEE, 2004. http://dx.doi.org/10.1049/cp:20040824.

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Rodrigues, Kathleen, Amanda Keen-Zebert, Sebastien Huot, and Ken Adams. "TESTING THE POTENTIAL OF THERMOLUMINESCENCE DATING OF VOLCANIC GLASS WITH KNOWN-AGE SAMPLES." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-308037.

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Musílek, Ladislav, Tomáš Polách, Tomáš Trojek, Anselmo Salles Paschoa, and Friedrich Steinhäusler. "Analysis of Potassium in Bricks—Determining the Dose Rate from [sup 40]K for Thermoluminescence Dating." In THE NATURAL RADIATION ENVIRONMENT: 8th International Symposium (NRE VIII). AIP, 2008. http://dx.doi.org/10.1063/1.2991242.

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Dies, J., F. Tarrasa, L. Miralles, C. De las Cuevas, and J. J. Pueyo. "Heating-Irradiation Experiments to Assess the System Bentonite-Carbon Steel in a Radioactive Waste Underground Storage Facility." In ASME 2001 8th International Conference on Radioactive Waste Management and Environmental Remediation. American Society of Mechanical Engineers, 2001. http://dx.doi.org/10.1115/icem2001-1238.

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Abstract One of the principal components of the engineered barrier system of a deep radioactive waste disposal in granite is the buffer, made of compacted bentonite blocks. Since the beginning of the operation of the repository the buffer will be subjected to a gamma radiation and temperature fields. Also, in some tens of years bentonite will be fully saturated. Cylindrical samples of saturated and compacted bentonite (200 mm in length and 50 mm in diameter) with embedded carbon steel discs, have been exposed to heat and radiation to assess their potential alteration under repository conditions. Two kinds of experiments were carried out. The first one was a heating experiment, called BIC-2A, in which the samples, bentonite and carbon steel discs, were subjected to a thermal gradient, ranging from 130°C to 90°C, during 120 days. The second one, named BIC-2B, was an irradiation and heating experiment, with the same time and temperature conditions than the BIC-2A, using a maximum dose rate of 3.5 kGy/h and a total absorbed dose of 10.5 MGy. The irradiation system consists of a set of six canisters, which hold the samples, placed between two cooper plates. These plates were subjected to a constant thermal gradient produced by a heating system driven by a PID controller, and consequently, the canisters were subjected to the same thermal gradient. Thermoresistances were used to control and monitor the temperature, whose evolution was stored on a computer. The canisters and the copper plates were placed inside a container that holds the system. High dose rates were achieved by placing the system inside the irradiation cell of an industrial irradiation facility, used to sterilise medical and pharmaceutical products with gamma rays produced by a 60Co source with a total activity of 300 000 Ci. Active and passive detectors were used to monitor dose and dose rate. An ionisation chamber was placed inside the container to obtain a continuous measure of the dose rate. The ionisation chamber was polarised and its signal measured by a picoammeter and the results stored on a computer. Moreover, several types of dosimeters were employed to measure the absorbed dose for several periods of time. Perspex, alanine and quartz dosemeters were used to measure low, intermediate and high doses. Either for the heating or for the heating-irradiation experiments, two cylinders were replaced by two new ones after two months of experimental running. Consequently, eight canisters were obtained at the end of each experiment, four canisters run during four months, and four additional canisters for two months. After basic manipulations, including a granulometrical separation, the bentonite samples were subjected to several mineralogical, chemical and physical analyses; namely, X-ray diffraction, X-ray fluorescence, Eh/pH measurements, and determinations of water content, cation exchange capacity, thermoluminescence response, electron spin resonance and oedometric tests. These analyses were carried out on a reference bentonite sample, which had not been heated nor irradiated, on the heated samples, and on the irradiated and heated samples, in order to discriminate which alterations are really due to what cause. The carbon steel discs, heated as well as irradiated and heated, were subjected to several metalographical analyses in order to assess the relevance of the corrosion processes that worked under these conditions.
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Reports on the topic "Quartz; Thermoluminescence dating; Thermoluminescence"

1

Berger, G. W., and J. L. Luternauer. Preliminary Fieldwork For Thermoluminescence Dating Studies At the Fraser River Delta, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/122559.

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