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首页> 外文期刊>Quaternary International >Dating sediments using potassium feldspar single-grain IRSL: Initial methodological considerations
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Dating sediments using potassium feldspar single-grain IRSL: Initial methodological considerations

机译:使用钾长石单粒IRSL进行沉积物测年:初始方法学上的考虑

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Potassium feldspar shows good potential for luminescence dating of Quaternary sediments in several locations assessed, including California, Tibet, Mongolia, Spain, Egypt, the UK, and New Zealand. In many of these locations, feldspar has particular importance owing to the low sensitivity of quartz OSL (optically stimulated luminescence) signals observed. Potassium feldspar-rich mineral fractions of sand-sized grains from a range of fluvial, alluvial, lake shoreline and glacial contexts were separated, and equivalent dose and fading determinations performed for single grains, besides conventional multiple-grain aliquots in some cases, using a protocol modified from a post-infra-red IRSL (infra-red stimulated luminescence) procedure. Most samples, but not all, contain a significant proportion of grains that provide IRSL signals sufficiently sensitive to determine equivalent dose values. Two main types of response have been observed. One group of samples displays regular behavior, with the majority of grains providing either a uniform equivalent dose (D_e) value for well-bleached samples, or a uniform minimum dose value with many higher values, presumably caused by incomplete zeroing. Uniform D_e values (or minimum values) suggest that the magnitude of signal reduction by anomalous fading for grains of different sensitivity is the same for all grains. A second common pattern of behavior is observed; for these samples, the minimum equivalent dose value is greater for grains with higher sensitivities. A surprising feature of this behavior for a subset of samples is an apparent saturating stretched exponential relationship between minimum equivalent dose and IRSL sensitivity. Samples in both groups contain rare grains with significantly lower D_e values, interpreted as intrusive grains, probably introduced by bio-turbation. This paper provides an initial survey of results, and briefly explores single-grain fading determination, besides comparisons of age estimates between different methods. An improved separation method to isolate the most sensitive grains referred to as "Super-K" is introduced, resulting in significant enhancement of the number of grains with bright IRSL signals.
机译:长石钾在被评估的多个地点(包括加利福尼亚,西藏,蒙古,西班牙,埃及,英国和新西兰)显示出良好的第四纪沉积物发光年代测定的潜力。在许多这些位置中,长石由于观察到的石英OSL(光学激发发光)信号的灵敏度低而特别重要。从一系列河流,冲积,湖岸和冰川环境中分离出富含钾长石的沙粒状颗粒的矿物级分,对单粒颗粒进行等效剂量和褪色测定,在某些情况下,除了常规的多谷物等分试样外,还使用从红外IRSL(红外激发发光)程序修改后的协议。大多数样品,但不是全部,都包含相当大比例的颗粒,这些颗粒提供的IRSL信号足够灵敏,可以确定等效剂量值。已经观察到两种主要类型的响应。一组样品显示出规律的行为,其中大多数谷物为漂白良好的样品提供统一的等效剂量(D_e)值,或者具有较高值的​​统一最小剂量值,这大概是由于不完全归零引起的。一致的D_e值(或最小值)表明,对于所有敏感度不同的晶粒,异常衰落导致的信号减弱幅度均相同。观察到第二种常见的行为模式。对于这些样品,具有更高灵敏度的谷物的最小当量剂量值更大。对于子集的样本,此行为的一个令人惊讶的特征是最小等效剂量与IRSL灵敏度之间存在明显的饱和拉伸指数关系。两组中的样品均含有D_e值明显较低的稀有晶粒,这被解释为侵入性晶粒,可能是由于生物扰动引起的。本文提供了结果的初步调查,并简要介绍了单粒衰落的确定方法,以及不同方法之间的年龄估计值的比较。引入了一种改进的分离方法以分离出称为“ Super-K”的最敏感晶粒,从而显着提高了具有明亮IRSL信号的晶粒的数量。

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