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Challenges involved in obtaining luminescence ages for long records of aridity: Examples from the Arabian Peninsula

机译:获取长期干旱记录的发光年龄所面临的挑战:阿拉伯半岛的例子

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In the last 35 years luminescence dating has provided a large database of ages for the deposition of dunes in desert environments. Over 380 ages have been generated for dunes from the Arabian Peninsula and demonstrate episodic dune deposition in the late Quaternary, but give a less clear pattern prior to similar to 50 ka. Interpreting databases of luminescence ages faces two issues. First, the precision of luminescence ages in the last 50 ka is between 5 and 10%, but for older ages the uncertainties may be much larger as luminescence signals reach saturation. Second, different luminescence signals from quartz and from feldspar have been used over the last 35 years as the method has developed and expanded. These different signals have different saturation limits and different rates at which they are reset by exposure to daylight at deposition. Approaches which focus on the most light sensitive signals (e.g. quartz OSL) are better suited to dating recent events, while those which show growth of the luminescence signal over the largest dose range (e.g. the thermally transferred OSL (TT-OSL) signal from quartz and the post-infrared infrared stimulated luminescence (pIR-IRSL) from feldspars) have the potential to date much older events. (C) 2016 Elsevier Ltd and INQUA. All rights reserved.
机译:在过去的35年中,发光测年为沙漠环境中沙丘的沉积提供了一个很大的年龄数据库。阿拉伯半岛的沙丘已经产生了380多个年龄,并显示了第四纪晚期的偶发性沙丘沉积,但在接近50 ka之前,其模式却不太清晰。解释发光年龄的数据库面临两个问题。首先,最近50 ka的发光年龄的精确度在5%到10%之间,但是对于较老的年龄,随着发光信号达到饱和,不确定性可能会更大。第二,随着方法的发展和扩展,过去35年以来一直使用来自石英和长石的不同发光信号。这些不同的信号具有不同的饱和度极限和通过沉积时暴露于日光而被重置的不同速率。重点放在对光最敏感的信号(例如石英OSL)上的方法更适合于对最近的事件进行约会,而那些在最大剂量范围内显示发光信号增长的方法(例如来自石英的热传递OSL(TT-OSL)信号)以及长石的红外后红外激发发光(pIR-IRSL)可能具有较早的事件发生的潜力。 (C)2016 Elsevier Ltd和INQUA。版权所有。

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