英国西南部的一个特里亚斯纪晚期撞击喷射层
Gordon Walkden1, Julian Parker, Simon Kelley
1Department of Geology and Petroleum Geology, Kings College, University of Aberdeen, Aberdeen AB24 3UD, UK. spherules@abdn.ac.uk
概括
研究人员在英国发现了一个特里亚斯纪撞击喷射层,其中含有球体和冲击石英. 这一发现为中生代期间的外星撞击提供了关键证据.
科学领域:
- 地质地质地质地质地质地
- 行星科学 行星科学
- 古生物学的古生物学
背景情况:
- 陆地撞击坑的记录很好,但相关的远端喷射沉积物在沉积物记录中很少见.
- 了解撞击事件需要识别和描述它们的喷射层.
研究的目的:
- 报告在英国西南部发现了一个重要的三叠纪撞击喷射沉积物的发现.
- 确定喷射层的日期,并将其与已知的撞击结构相关联.
- 分析这一发现对理解中生代冲击和灭绝的影响.
主要方法:
- 在英国西南部进行地质实地工作,以识别和采样沉积物沉积物.
- 显微镜分析以识别特有的冲击球体和冲击石英.
- 在喷射层内地的阿贡-阿贡测年.
主要成果:
- 识别了含有球体和冲击石英的三叠纪沉积沉积物,表明了撞击喷射层.
- 阿贡-阿贡约会给出了该沉积物214 +/- 250万年的年龄.
- 这个年龄与几个三叠纪撞击坑相吻合,尤其是Manicouagan和Rochechouart.
结论:
- 发现的沉积物代表了中生代外星撞击的罕见沉积物记录.
- 这一发现有助于破译撞击事件的频率,影响和动态.
- 进一步的研究可以探索这种喷射层与化石灭绝的时间之间的关系.
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