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Ubiquity of anomalous fading in K-feldspars and the measurement and correction for it in optical dating

机译:钾长石异常衰落的普遍性及其在光学测年中的测量与校正

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Anomalous-fading rates were measured in K-feldspars separated from 49 sediment samples, mainly from North America. The intensity of the optically stimulated luminescence was found to decrease linearly with the logarithm of time since irradiation between 2 days and approx 1 year of storage at room temperature. Anomalous-fading rates ranged from 2 percent to 10 percent per decade, a decade being a factor of 10 in time since irradiation. The sample provenances were sufficiently varied that anomalous fading appears to be ubiquitous. We have experimented with correction of optical ages for anomalous fading on the assumption that the observed fading can be extrapolated a further four decades in time. The corrected ages are in satisfactory agreement with independent ages. These results are restricted to the low-dose region of the dose response and are not expected to be applicable to samples older that approx 20-50 ka.
机译:在从49个沉积物样本(主要来自北美)中分离出的钾长石中,测量了异常褪色率。发现自在室温下储存2天至大约1年之间照射以来,光激发的发光强度随时间的对数线性降低。异常衰落率范围为每十年2%到10%,十年是自辐射以来时间的10倍。样本出处足够多,异常褪色似乎无处不在。我们已经对光学衰落进行了实验,以校正异常衰落,但前提是可以将观察到的衰落再推断出四十年的时间。校正后的年龄与独立年龄相符。这些结果仅限于剂量反应的低剂量区域,预计不适用于年龄约20-50 ka的样品。

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