首页> 美国卫生研究院文献>Methods and Protocols >Single Aliquot Regeneration (SAR) Optically Stimulated Luminescence Dating Protocols Using Different Grain-Sizes of Quartz: Revisiting the Chronology of Mircea Vodă Loess-Paleosol Master Section (Romania)
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Single Aliquot Regeneration (SAR) Optically Stimulated Luminescence Dating Protocols Using Different Grain-Sizes of Quartz: Revisiting the Chronology of Mircea Vodă Loess-Paleosol Master Section (Romania)

机译:单等分试样再生(SAR)光激发的发光约会协议使用不同晶粒度的石英:重新研究MirceaVodăLoess-Paleosol主分区(罗马尼亚)的年代

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摘要

The loess-paleosol archive from Mircea Vodă (Romania) represents one of the most studied sections in Europe. We are applying here the current state of the art luminescence dating protocols for revisiting the chronology of this section. Analysis were performed on fine (4–11 µm) and coarse (63–90 µm) quartz extracts using the single aliquot regenerative (SAR) optically stimulated luminescence (OSL) dating protocol. Laboratory generated SAR dose response curves in the high dose range (5 kGy for fine quartz and 2 kGy for coarse quartz) were investigated by employing a test dose of either 17 or 170 Gy. The results confirm the previously reported different saturation characteristics of the two quartz fractions, with no evident dependency of the equivalent dose (D ) on the size of the test dose. The OSL SAR ages are discussed and compared to the previously obtained results on quartz and feldspars. The previous reports regarding the chronological discrepancy between the two quartz fractions are confirmed. However, while previous investigations on other sites concluded that this discrepancy appears only above equivalent doses of about 100 Gy, here fine grain quartz ages underestimate coarse quartz ages starting with equivalent doses as low as around 50 Gy.
机译:来自MirceaVodă(罗马尼亚)的黄土古土壤档案是欧洲研究最多的地区之一。我们在此应用最新的发光测年协议,以重新讨论本节的时间顺序。使用单等份再生(SAR)光激发发光(OSL)测年方案对细(4-11 µm)和粗(63-90 µm)石英提取物进行了分析。通过使用17或170 Gy的测试剂量,研究了实验室在高剂量范围(细石英为5 kGy,粗石英为2 kGy)中产生的SAR剂量响应曲线。结果证实了先前报道的两个石英级分的不同饱和特性,等效剂量(D)对测试剂量的大小没有明显的依赖性。讨论了OSL SAR年龄,并将其与先前在石英和长石上获得的结果进行了比较。先前关于两个石英级分之间时间差异的报道得到确认。但是,尽管先前在其他站点进行的调查得出结论,这种差异仅出现在大约100 Gy的等效剂量以上,但此处的细晶粒石英年龄低至等效剂量低至约50 Gy时低估了粗石英年龄。

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