概括
研究人员使用抛光石切片开发了一种新的热发光测年方法,提高了石和石的火化测年准确度,可追溯到公元前30万年.
科学领域:
- 考古学测量是指考古学测量的方法.
- 地质时间学 (Geochronology)
- 发光 发光 约会 约会
背景情况:
- 石等燃烧材料的热发光 (TL) 测年对于考古学和地质学研究至关重要.
- 使用粉样样本的传统方法受到三热发光和再生热发光的干扰,限制了准确性.
研究的目的:
- 为了完善燃烧石的热发光测年技术.
- 为了消除干扰的发光信号,以便更准确地确定年龄.
- 建立一个可靠的方法来测定chert和石灰岩碎片的年代.
主要方法:
- 在热发光测量中使用薄,抛光的烧石片,而不是粉末.
- 测量内部和外部辐射剂量速率.
- 将该方法应用于西班牙卡里古埃拉的考古样本.
主要成果:
- 消除来自三热发光和再生热发光的干扰.
- 对石和石碎片的火解的准确绝对约会 (10-15%的准确性).
- 考古样本的约会时间为公元前12,000年至50,000年. (古石器时代晚期 - - 史前石器时代到穆斯特时代) 和一个铜器时代标本在公元前4300年.
结论:
- 抛光切片方法显著提高了燃烧石的热发光测年方法的可靠性.
- 这种技术为高达公元前30万年的材料提供了准确的地质年代数据.
- 该方法通过与考古样本的其他约会技术一致的结果来验证.
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