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Low temperature thermochronology using thermoluminescence signals from K-feldspar

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Figure 1

Typical luminescence signals from sample N-1. A) Thermoluminescence (TL); B) Isothermal thermoluminescence (ITL).
Typical luminescence signals from sample N-1. A) Thermoluminescence (TL); B) Isothermal thermoluminescence (ITL).

Figure 2

Schematic running sequences of luminescence protocols. A) MAA-TL, B) MAR-TL, C) MAA-ITL, D) MAR-ITL and E) SAR-ITL protocols.
Schematic running sequences of luminescence protocols. A) MAA-TL, B) MAR-TL, C) MAA-ITL, D) MAR-ITL and E) SAR-ITL protocols.

Figure 3

Typical growth (dose response) curves of the luminescence signals of protocols. A) MAA-TL, B) MAR-TL, C)MAA-ITL, D) MAR-ITL and E) SAR-ITL protocols.
Typical growth (dose response) curves of the luminescence signals of protocols. A) MAA-TL, B) MAR-TL, C)MAA-ITL, D) MAR-ITL and E) SAR-ITL protocols.

Figure 4

The SAR-ITL protocol dose recovery test results.
The SAR-ITL protocol dose recovery test results.

Figure 5

Comparison of K-feldspar De results of the MAA-TL, MAR-TL, MAA-ITL, MAR-ITL and SAR-ITL protocols.
Comparison of K-feldspar De results of the MAA-TL, MAR-TL, MAA-ITL, MAR-ITL and SAR-ITL protocols.

Evaluation form of MAA-TL, MAR-TL, MAA-ITL, MAR-ITL and SAR-ITL protocols.

MAA-TLMAR-TLMAA-ITLMAR-ITLSAR-ITL
TL peaks (geothermometers) can be measured in one run
Well studied kinetics parameters
Multiple aliquots protocol requires shorter machine time
TL glow curves indicate the thermal stability
Overcome weak ITL signals problem
Sensitivity change of reheating can be minimized
Apply to ITL signals components fitting
Don’t need normalization
Avoid overlapping TL peaks
Overcome the atmosphere protection of the TL oven
Overcome blackbody radiation
Need less sample materials
Obtain De by interpolation from growth curve
Advantage ✓Disadvantage ✘

Fugong valley samples De results determined using MAR-TL and SAR-ITL protocols.

SampleDe of MAR-TL (Gy)De of SAR-ITL (Gy)
At 250°CAt 260°CAt 270°CAt 280°CAt 290°CAt 300°CAt 310°CAt 320°CAt 330°CAt 235°CAt 255°C
FG-A23.9±3.133.7±4.850.1±7.576.9±11.2116.5±15.2167.6±19.5227.2±23.8287.5±27.1342.4±30.956.1±12.3146.0±9.1
FG-B20.8±2.830.1±4.247.3±6.477.0±9.5123.6±13.2189.5±16.6271.2±19.4361.4±21.7449.9±23.673.7±11.2203.7±15.6
FG-C29.5±3.743.1±5.665.2±8.299.4±11.5147.9±14.8209.1±16.8276.1±17.1340.4±16.3395.1±17.1109.8±7.0243.2±14.5
eISSN:
1897-1695
Langue:
Anglais
Périodicité:
Volume Open
Sujets de la revue:
Geosciences, other