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Coarse versus fine-grain quartz optical dating of the sediments related to the 1985 Ms7.1 Wuqia earthquake, northeastern margin of the Pamir salient, China Cover

Coarse versus fine-grain quartz optical dating of the sediments related to the 1985 Ms7.1 Wuqia earthquake, northeastern margin of the Pamir salient, China

Open Access
|Nov 2017
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Figures & tables

Fig. 1

Aster image showing regional tectonic structure, the 1985 Wuqia earthquake surface rupture and trench location. Modified from Li et al. (2012).

Fig. 2

Location of the modern sample LED11-7 (Left); Trench wall showing the location of samples LED11-1, 11-2 and 11-6 (Right).

Fig. 3

Luminescence characteristics. a – Quartz purity IR check; b – Dose recovery as a function of preheat temperature for coarse grains quartz; c – OSL decay curves for single quartz grains from sample LED11-1, the inset shows a corresponding dose response curve (DRC), the red point is recycling point; d – A histogram of dose recovery ratios for single quartz grains using a 10 s preheat at 260°C for and a 220°C cutheat.

Fig. 4

a – Sensitivity-corrected multiple aliquot regenerative-dose growth curve (SMAR) of sample LED11-1; b – OSL decay curves of sample LED11-1; c – A SAR growth curve; d – Coarse grain quartz small aliquot standardized growth curve (SA-DRC). The red diamonds are sample-specific and were projected on the SA-DRC.

Table 1

Dose rate results for the samples.

Sample No.Depth (m)U (ppm)Th (ppm)K (%)Water contenta (%)Dose rate (Gy/ka)
CQFQ
LED11-12.41.655.31.375 ± 52.1 ± 0.12.9 ± 0.2
LED11-22.81.744.841.155 ± 52.0 ± 0.12.6 ± 0.1
LED11-60.61.967.751.492 ± 22.7 ± 0.23.4 ± 0.2
LED11-70.21.354.671.22 ± 22.1 ± 0.12.5 ± 0.1

a Water contents were estimated at 5 ± 5% or 2 ± 2%

Table 2

De values of single grains, small aliquot SA-SGC and fine grains for the samples shown on Fig 2.

Sample No.Single grainsSmall aliquot SA-SGCFine grains
n/NaPb (%)ODc (%)Ded (Gy)Age (ka)n/NaPb (%)ODc (%)Ded (Gy)Age (ka)De (Gy)Age (ka)
LED11-1158/48003.34514.3−1.7+1.96.7−0.9+1.043/78553614.3−3.0+3.36.7−1.5+1.665.7 ± 5.422.9 ± 1.9
LED11-255/23002.4629.6−1.9+2.54.9−1.0+1.363/14244599.8−1.8+3.05.0−1.0+1.6157.6 ± 14.360.5 ± 5.4
LED11-655/37001.5455.2−1.0+1.42.0−0.4+0.552/14440335.4−0.5+1.12.0−0.2+0.666.8 ± 3.119.5 ± 0.9
LED11-753/18002.9800.2−0.1+0.20.1−0.05+0.142/8847590.3−0.2+0.30.15−0.1+0.157.0 ± 0.32.8 ± 0.1

a n represents the number of accepted single grains or small aliquots that passed the SAR rejection criteria and used for De determination, N represents total number of grains or aliquots measured;

b Proportion (%) of the grains or aliquots that have a detectable OSL signal;

c over-dispersion;

d De obtained using the minimum age model.

a n represents the number of accepted single grains or small aliquots that passed the SAR rejection criteria and used for De determination, N represents total number of grains or aliquots measured;

b Proportion (%) of the grains or aliquots that have a detectable OSL signal;

c over-dispersion;

d De obtained using the minimum age model.

Fig. 5

Radial plots and KDE plots from single grains (SG) and small aliquot standardised growth curve (SA-SGC) for samples LED11-1, LED11-2 and LED11-6. Grey bands on radial plots show the samples’ De values with 2-sigma error (Table 2). Only KDE plots are shown for the sample LED11-7.

DOI: https://doi.org/10.1515/geochr-2015-0075 | Journal eISSN: 1897-1695 | Journal ISSN: 1733-8387
Language: English
Page range: 299 - 306
Submitted on: Jan 31, 2016
Accepted on: May 19, 2017
Published on: Nov 23, 2017
Published by: Sciendo
In partnership with: Paradigm Publishing Services

© 2017 Huili Yang, Jie Chen, Naomi Porat, Tao Li, Wenqiao Li, Weipeng Xiao, published by Sciendo
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.