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Exploring complexity in luminescence dating of quartz and feldspars at the Middle Stone Age site of Mwulu's cave (Limpopo, South Africa)

机译:探讨MWULU洞穴中石龄地区石英和长石的发光约会的复杂性(南非林普帕波波)

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摘要

Luminescence dating is applied to sediments from Mwulu's Cave, whose lithics have been typologically considered Middle Stone Age (MSA) and have been previously assigned to what is called the Pietersburg industry. This industry is, however, poorly defined both chronologically and typologically. Luminescence methods were applied to both quartz and potassium feldspars by two different laboratories. Age results from single-grain quartz are much younger than those from multi-grain aliquots and this is attributed to the use of different fits to the growth curves and the effect of this on samples near saturation. Single-grain potassium feldspar ages are much older than the single-grain quartz ages. Application of various methods to address anomalous fading produced broadly consistent results among samples. Most K-feldspar samples appear to be about 90 ka. These are compared to other South African MSA sequences and industries.
机译:发光约会适用于Mwulu洞穴的沉积物,其岩石是在线上被认为是中间的石头年龄(MSA),并以前分配到被称为Pietberburg行业的内容。 然而,该行业是以时间和类型计算的差异不足。 用两种不同的实验室应用了发光方法对石英和钾长石。 单粒石英的年龄结果比来自多谷物等分试样的更年轻,这归因于使用不同的拟合对生长曲线的使用以及对饱和度附近的样品的影响。 单粒钾长石年龄比单粒石英年龄较大。 在寻址异常衰落的各种方法的应用在样品中产生了广泛一致的结果。 大多数K-feldspar样本似乎约为90 ka。 这些与其他南非MSA序列和行业进行了比较。

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