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Extending the area of investigation of fine versus coarse quartz optical ages from the Lower Danube to the Carpathian

机译:将细石英和粗石英光学年龄的研究范围从下多瑙河扩展到喀尔巴阡山脉

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Despite the general satisfactory performance of quartz in the single aliquot regeneration protocol (SAR), previous optically stimulated luminescence (OSL) dating studies of key loess sections in Romania, Lower Danube region, revealed a disturbing disagreement among the ages obtained on fine (4-11 mu m) grains and coarse (63-90 mu m) grains respectively. The current study aims at expanding these investigations, both by extending the area of study from the Lower Danube Basin to the Carpathian Basin and by applying time-resolved optically stimulated luminescence (TR-OSL) on quartz, in order to gain further insights into the above mentioned behaviour. The samples from the Orlovat loess paleosol section (Vojvodina, Serbia) showed a similar behaviour to that previously reported on Romanian loess. A marked difference between the dose saturation characteristics of fine and coarse quartz OSL signals is observed for both continuous wave (CW-OSL) and pulsed OSL (POSL), where the dose response (up to 1000 Gy) is well described by a sum of two saturating exponential functions. TR-OSL measurements show one single, characteristic quartz lifetime for both natural as well as regenerative signals in the entire dose range investigated. A general disagreement between the ages obtained on the two grain sizes for samples with equivalent doses higher than about 100 Gy is reported as in the case of Romanian loess, inferring that the age discrepancy between the two grain sizes might be more widespread than previously thought. (C) 2014 Elsevier Ltd and INQUA. All rights reserved.
机译:尽管在单一等分试样再生协议(SAR)中石英的总体性能令人满意,但先前在下多瑙河地区罗马尼亚的主要黄土剖面上进行的光激发发光(OSL)测年研究显示,在细碎条件下获得的年龄之间存在令人不安的分歧(4-颗粒分别为11微米和63-90微米。当前的研究旨在通过将研究范围从下多瑙河盆地扩展到喀尔巴阡盆地以及通过在石英上应用时间分辨的光激发发光(TR-OSL)来扩大这些研究范围,以便进一步了解上述行为。 Orlovat黄土古土壤剖面(塞尔维亚Vojvodina)的样品显示出与先前报道的罗马尼亚黄土相似的行为。对于连续波(CW-OSL)和脉冲OSL(POSL)都可以观察到细石英OSL信号和粗石英OSL信号的剂量饱和特性之间存在明显差异,其中剂量响应(最大1000 Gy)可以用以下公式的总和来很好地描述:两个饱和指数函数。 TR-OSL测量显示了在整个研究剂量范围内,天然信号和再生信号的单一特征石英寿命。对于罗马尼亚黄土,等效剂量高于约100 Gy的样品在两种粒度上获得的年龄之间普遍存在分歧,这表明两种粒度之间的年龄差异可能比以前认为的更为普遍。 (C)2014 Elsevier Ltd和INQUA。版权所有。

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