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Ultrafast Component Effects on Quartz Single Grains Dose Estimation from Khutagt Uul Mountains, Mongolia

Saran Tengis

Saran Tengis

Institute of Physics and Technology, Mongolian Academy of SciencesUlaanbaatar, Mongolia
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Tengis, Saran
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Saran Solongo

Saran Solongo

Institute of Physics and Technology, Mongolian Academy of SciencesUlaanbaatar, Mongolia
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Solongo, Saran
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Rinchinkhorol Munkhtulga

Rinchinkhorol Munkhtulga

Institute of History and Archaeology, Mongolian Academy of SciencesUlaanbaatar, Mongolia
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Munkhtulga, Rinchinkhorol
  
Dec 31, 2021
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Article Category: Conference Proceedings of the 5Asia Pacific Luminescence and Electron Spin Resonance Dating Conference October 15–17, 2018, Beijing, China. Guest Editor: Barbara Mauz
Published Online: Dec 31, 2021
Page range: 263 - 271
Received: Feb 15, 2019
Accepted: Jul 12, 2019
DOI: https://doi.org/10.1515/geochr-2015-0117
Keywords
© 2019 Saran Tengis et al., published by Sciendo
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

Fig. 1

The dose-response curves for individual quartz grains of the heated quartz sample L-EVA1201, showing Lx/Tx as a function of regeneration doses. The corresponding luminescence decay curves from the individual grains are shown on the right side: natural OSL (N – black line), test dose (T1 – red line and T after IRSL – blue line) OSL decay curves as a function of stimulation time obtained from single grains. In addition, the corresponding TL measured from the aliquot at the end of the SAR protocol served as additional criteria for examining the presence of feldspar.
The dose-response curves for individual quartz grains of the heated quartz sample L-EVA1201, showing Lx/Tx as a function of regeneration doses. The corresponding luminescence decay curves from the individual grains are shown on the right side: natural OSL (N – black line), test dose (T1 – red line and T after IRSL – blue line) OSL decay curves as a function of stimulation time obtained from single grains. In addition, the corresponding TL measured from the aliquot at the end of the SAR protocol served as additional criteria for examining the presence of feldspar.

Fig. 2

a) and c) The dose-response curves for individual quartz grains of the sedimentary quartz L-EVA1202, showing Lx/Tx as a function of regeneration doses. The corresponding luminescence decay curves from the individual grains are shown on the right side: natural OSL (N – blue line), test dose (T1 – red line and T after IRSL – blue line) OSL decay curves as a function of stimulation time obtained from single grains. In addition, LM-OSL from a bright grain (e) indicated the presence of a significant slow component in addition to the fast component; however those bright grains were rejected.
a) and c) The dose-response curves for individual quartz grains of the sedimentary quartz L-EVA1202, showing Lx/Tx as a function of regeneration doses. The corresponding luminescence decay curves from the individual grains are shown on the right side: natural OSL (N – blue line), test dose (T1 – red line and T after IRSL – blue line) OSL decay curves as a function of stimulation time obtained from single grains. In addition, LM-OSL from a bright grain (e) indicated the presence of a significant slow component in addition to the fast component; however those bright grains were rejected.

Fig. 3

Effect of precision on De a). for sample L-EVA1201. Central Age Model (CAM, squares) dose and the relative standard error (as circles) on CAM De; b). for sample L-EVA1202. FMM and MAM De (triangles and squares) as function of precision on De.
Effect of precision on De a). for sample L-EVA1201. Central Age Model (CAM, squares) dose and the relative standard error (as circles) on CAM De; b). for sample L-EVA1202. FMM and MAM De (triangles and squares) as function of precision on De.

Fig. 4

a) The fitting results for pottery L-EVA1201, and for sedimentary quartz LEVA1202 showing the presence of UF, F and medium OSL components. b) The corresponding constant and increasing De-t-plots for L-EVA1201 and L_EVA1202 are shown.
a) The fitting results for pottery L-EVA1201, and for sedimentary quartz LEVA1202 showing the presence of UF, F and medium OSL components. b) The corresponding constant and increasing De-t-plots for L-EVA1201 and L_EVA1202 are shown.

Fig. 5

Growth curves for naturally sedimentary and heated quartz grains.
Growth curves for naturally sedimentary and heated quartz grains.

Fig. 6

Radial plots of the single grain dose distributions a) fast De from accepted 167 grains (closed triangles) for heated quartz L-EVA1201 and UF De from n = 159 (circles). The solid grey band is centered on the weighted mean, De determined using Central Age Model, over-dispersion of 14.7%. b) De from accepted 134 grains of L-EVA1202 channels 6–9. The solid grey lines indicate the CAM De = 15.13 ± 1.47 Gy and overdispersion of 96.8%. MAM De = 5.91±1.38 Gy.
Radial plots of the single grain dose distributions a) fast De from accepted 167 grains (closed triangles) for heated quartz L-EVA1201 and UF De from n = 159 (circles). The solid grey band is centered on the weighted mean, De determined using Central Age Model, over-dispersion of 14.7%. b) De from accepted 134 grains of L-EVA1202 channels 6–9. The solid grey lines indicate the CAM De = 15.13 ± 1.47 Gy and overdispersion of 96.8%. MAM De = 5.91±1.38 Gy.
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