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Comparison of paired quartz OSL and feldspar post-IR IRSL dose distributions in poorly bleached fluvial sediments from South Africa

机译:成对石英OsL和长石后红外IRsL剂量分布在南非贫瘠河流沉积物中的比较

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摘要

A comparative study using quartz optically stimulated luminescence (OSL) and feldspar post-infrared infrared stimulated luminescence (post-IR IRSL) was undertaken on Quaternary fluvial sediments from an unnamed tributary of the Moopetsi River in South Africa. The aim is to assess whether the post-IR IRSL signal can be used to date incompletely bleached sediments. Several post-IR IRSL signals using varying stimulation and preheat temperatures were investigated; of these the post-IR IRSL225 signal was deemed most appropriate for dating because it bleached most rapidly. The feldspar post-IR IRSL225 equivalent dose (De) values from this site are consistently larger than those from quartz OSL, probably due to differences in the bleaching characteristics of the two signals. Additionally, the post-IR IRSL225 De values within a sample showed less variation in precision than the quartz De data, possibly due to greater averaging between grains in the feldspar small aliquots. The agreement between ages based on the OSL and post-IR IRSL225 signals was better for younger samples (<20 ka) than for older ones (>50 ka); the cause of this variation is unclear.
机译:对来自南非莫普切河的一个未命名支流的第四纪河流沉积物进行了比较研究,该研究使用石英光学激发发光(OSL)和长石红外后红外激发发光(IR IRSL)。目的是评估IR-IRSL后信号是否可用于确定未完全漂白的沉积物的年代。研究了几个使用变化的刺激和预热温度的IR后IRSL信号;这些后IR IRSL225信号被认为最适合约会,因为它漂白得最快。该位置的长石IR IRSL225等效剂量(De)值始终大于石英OSL的长石,这可能是由于两个信号的漂白特性不同所致。此外,样品中的IR后IRSL225 De值显示的精度变化要比石英De数据小,这可能是由于长石小等分试样中晶粒之间的平均程度更高。基于OSL和IR IR225225后信号的年龄之间的一致性对于较年轻的样本(<20 ka)优于较老的样本(> 50 ka);这种变化的原因尚不清楚。

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