概括
陶器碎片中的高矿石颗粒使用裂变轨道测绘来识别. 这些发现突出了放射性颗粒对于热发光和α-反弹轨道测年方法的潜力.
科学领域:
- 地质化学 地质化学
- 考古测量考古测量方法
- 材料科学 材料科学 材料科学
背景情况:
- 陶器碎片含有矿物质含,可以保存时间信息.
- 富含的矿物颗粒是潜在的计时器,因为它们具有放射性衰变特性.
研究的目的:
- 在来自不同地理来源的陶碎片中定位和识别高矿石颗粒.
- 评估这些已识别的颗粒是否适合使用先进的约会技术.
主要方法:
- 诱导裂变轨道测绘被用来检测富含的微粒.
- 扫描电子显微镜与微探针分析被用于矿物识别 (石,阿帕).
主要成果:
- 在陶碎片中成功地发现了高度 (100-3000 ppm) 的小矿物颗粒 (10-50 微米).
- 鉴定到的颗粒主要是石和石.
结论:
- 放射性矿物质颗粒,如石和石,存在于陶器中.
- 这些颗粒为热发光测年和α-反弹轨道测年应用提供了显著的优势.
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