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Monitoring anomalous fading of TL of feldspars by using far-red emission as a gauge

机译:以远红光为指标监测长石TL异常衰落

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摘要

TL dating of Feldspars of volcanic origin is thwarted by anomalous fading of its emission in the usual spectral range from UV to red, though in the far-red range it has been shown to be stable. A new method of evaluation of this anomalous fading is proposed. The comparison is no longer made directly between total TL emissions after different storage limes. Instead, TL is first measured in two spectral ranges simultaneously, the 'blue' one, usually monitored For fading, and the far-red one. Secondly, at every temperature the ratio of 'blue' to far-red, named B-ir, is computed. Thirdly, to monitor anomalous fading, these ratios are compared between different TLs. When fading shows, values of B-ir are observed to decrease during storage, according to the logarithmic law, down to very low values. A temperature dependance of anomalous fading is firmly established. (C) 2000 Elsevier Science Ltd. All rights reserved. [References: 12]
机译:火山起源的长石的TL测年在通常的光谱范围(从紫外线到红色)中的发射异常衰减,阻碍了它的发散,尽管在远红色范围中,它已被证明是稳定的。提出了一种评估这种异常衰落的新方法。在存储石灰不同之后,不再直接在总TL排放之间进行比较。取而代之的是,首先在两个光谱范围内同时测量TL,通常在衰落时对其进行监视的“蓝色”光谱域和远红色光谱域。其次,在每个温度下,计算“蓝”与远红之比(称为B-ir)。第三,为了监视异常衰落,在不同的TL之间比较这些比率。当显示衰落时,根据对数定律,观察到B-ir的值在存储过程中降低,降至非常低的值。牢固建立了温度依赖于异常衰落。 (C)2000 Elsevier ScienceLtd。保留所有权利。 [参考:12]

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