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Luminescence dating of K-feldspar from sediments: A protocol without anomalous fading correction

机译:沉积物中钾长石的发光测年:无异常衰落校正的方案

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摘要

A protocol for optical dating of potassium-rich feldspar (K-feldspar) is proposed. It utilizes the infrared stimulated luminescence (IRSL) signal measured by progressively increasing the stimulation temperature from 50 to 250 °C in step of 50 °C, so-called multi-elevated-temperature post-IR IRSL (MET-pIRIR) measurements. Negligible anomalous fading was observed for the MET-pIRIR signals obtained at 200 and 250 °C. This was supported by equivalent dose (D_e) measurements using the IRSL and MET-pIRIR signals. The D_e values increase progressively from 50 °C to 200 °C, but similar D_e values were obtained for the MET-pIRIR signal at 200 and 250 °C. Measurement of modern samples and bleached samples indicates that the MET-pIRIR signals have small residual doses less than 5 Gy equivalent to about 1-2 ka. We have tested the protocol using various sedimentary samples with different ages from different regions of China. The MET-pIR IRSL ages obtained at 200 and 250 °C are consistent with independent and/or quartz OSL ages.
机译:提出了富钾长石(K-长石)光学测年的协议。它利用红外刺激发光(IRSL)信号,该信号是通过将刺激温度从50°C逐步增加到50°C逐步增加到50°C来测量的,即所谓的多次高温后IR IRSL(MET-pIRIR)测量。对于在200和250°C下获得的MET-pIRIR信号观察到的异常衰落可忽略不计。使用IRSL和MET-pIRIR信号的等效剂量(D_e)测量支持了这一点。 D_e值从50°C逐渐增加到200°C,但是对于MET-pIRIR信号在200和250°C时获得了相似的D_e值。对现代样品和漂白样品的测量表明,MET-pIRIR信号具有小于5 Gy的小残留剂量,相当于约1-2 ka。我们已经使用来自中国不同地区的不同年龄的各种沉积物样品对协议进行了测试。在200和250°C下获得的MET-pIR IRSL年龄与独立和/或石英OSL年龄一致。

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