概括
研究人员使用碳-14原子计数来测定犹他州史前地震相关的木炭的年代. 这为瓦萨奇断层的古代地震事件提供了新的年龄估计,从7,800年前到9,000年前.
科学领域:
- 地质地质地质地质地质地
- 古代地震学 (paleoseismology) 是一种古地震学.
- 射线测量约会的方法
背景情况:
- 犹他州的瓦萨奇断层是一个重要的地质特征,有史前地震的历史.
- 了解过去地震事件的时间对于地震危险评估至关重要.
研究的目的:
- 为了确定与瓦萨奇断层相关的史前地震的年龄.
- 在地质样本上应用先进的约会技术.
主要方法:
- 直接计数碳-14 (14C) 的原子,使用一个Vand de Graaff双重加速器.
- 从土壤层中采集的毫克大小的破碎木炭样本的放射测年.
主要成果:
- 对于与史前地震有关的土壤层,确定了7,800,8,800和9000年前的年龄.
- 约会给出了一个不确定性的+/- 600年每个年龄的确定.
结论:
- 该研究成功地确定了与瓦萨奇断层史前地震活动相关的木炭的年代.
- 这些发现为了解该地区的地震历史提供了宝贵的时间数据.
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