Effect of related parameters on exposure age and erosion rate obtained via rock surface luminescence dating

Ming LUO; Zhijun GONG; Fusheng GUO; Huaming PENG

doi:10.11889/j.0253-3219.2024.hjs.47.010002

Journals >NUCLEAR TECHNIQUES >Volume 47 >Issue 1 >Page 010002 > Article

NUCLEAR TECHNIQUES
Vol. 47, Issue 1, 010002 (2024)

Ming LUO^1、2、3, Zhijun GONG^1、*, Fusheng GUO¹, and Huaming PENG¹

Author Affiliations

¹School of Earth Sciences, East China University of Technology, Nanchang 330013, China

²Key Laboratory for Digital Land and Resources of Jiangxi Province, East China University of Technology, Nanchang 330013, China

³State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China

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DOI: 10.11889/j.0253-3219.2024.hjs.47.010002 Cite this Article

Ming LUO, Zhijun GONG, Fusheng GUO, Huaming PENG. Effect of related parameters on exposure age and erosion rate obtained via rock surface luminescence dating[J]. NUCLEAR TECHNIQUES, 2024, 47(1): 010002 Copy Citation Text

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Simulated the residual luminescence-depth profiles as predicted using Eqs.(4) and (7) for rock surfaces having different exposure ages (a) and erosion rates (b), respectively

Fig. 1. Simulated the residual luminescence-depth profiles as predicted using Eqs.(4) and (7) for rock surfaces having different exposure ages (a) and erosion rates (b), respectively

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Relationship between the depth of half saturation (the depth at which the luminescence signal is 50% of the saturation level) and exposure time under different parameter values. Only one of the following parameters were varied while keeping the other parameters unchanged: (a) μ, (b) σφ0¯, (c) D˙, (d) D0.

Fig. 2. Relationship between the depth of half saturation (the depth at which the luminescence signal is 50% of the saturation level) and exposure time under different parameter values. Only one of the following parameters were varied while keeping the other parameters unchanged: (a) μ, (b)

\bar{σ φ_{0}}

, (c)

\dot{D}

, (d) D₀.

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Fig. 3. Relationship between the depth of half saturation and exposure age of typical granite gneiss (circle) and sandstone (triangle)

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Fig. 4. Relationship between the depth of half saturation and erosion rate under different parameter values. Only one of the following parameters are varied while keeping the other parameters unchanged: (a) μ, (b)

\bar{σ φ_{0}}

, (c) D₀, (d)

\dot{D}

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样品名 Sample name	岩性 Lithology	表面颜色 Surface color	采样位置 Sampling location	μ / mm^-1	$\bar{σ φ_{0}}$ / ka^-1	$\dot{D}$ / Gy∙ka^-1	D₀ / Gy	释光信号 Luminescence signal	参考文献 References
2014KZ4	细砂岩 Fine sandstone	紫红色 Purplish red	中国新疆 Xinjiang province in China	2.43±0.48	(1.1±1.9)×10³			IR₅₀	[27]
HS-OSL-29	砂岩 Sandstone	土黄色* Khaki*	美国犹他州 Utah, USA	1.01±0.02	214±19			IR₅₀	[1]
CO-01	砂岩 Sandstone	灰色 Grey	英国 Britain	2.86±0.60	―			pIRIR₂₂₅	[6]
―	富长石花岗岩 Feldspar-rich granite	红褐色* Reddish brown*	丹麦奥胡斯 Aarhus, Denmark	0.72±0.07	(5±2)×10³	6.0±0.2	280±30	IR₅₀	[4]
MBTP1	花岗岩 Granite	灰白色* Grey white*	欧洲阿尔卑斯 European Alps	0.596	129×10³	8	500	IR₅₀	[28]
1 K	花岗岩 Granite	肉红色 Flesh pink	中国内蒙古 Inner Mongolia, China	1.10 ±0.19	2 631±14	3.3±0.2	506.0±15.5	pIRIR₁₇₅	[22]
GG18-05-01	片岩 Schist	―	瑞士 Switzerland	1.6	4 900			pIRIR₂₂₅	[20]
MUZTAGH-2	花岗片麻岩 Granitic gneiss	青灰色* Cinerrous*	新疆帕米尔 Chinese Pamir	0.59±0.01	2 165±51	5.45±0.09	238±34	IR₅₀	[2]
MZ051S-3	片麻岩 Gneiss	灰黑色* Dark gray*	意大利北部 Northern Italy	0.91±0.16	―		430±30	IR₅₀	[29]
GZ5(2)	片麻岩 Gneiss	灰黑色* Dark gray *	新疆帕米尔 Chinese Pamir	1.05±0.02	(11±1)×10³			MET-pIRIR₁₇₀	[17]

Table 1. Statistics on the bleaching parameters of luminescence signals in the literature

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