概括
来自基拉韦亚火山的深海玄武岩的放射性和约会产生了高达2200万年的年龄. 这些发现提醒人们不要在海洋底传播研究中使用深海玄武岩日期.
科学领域:
- 地质化学 地质化学
- 海洋地质 海洋地质学
- 火山学 火山学是一门学科.
背景情况:
- 深海玄武岩对于理解地球的地质历史至关重要.
- 这些玄武岩的精确约会对于板块构造学和海洋底扩散研究至关重要.
- 基拉韦亚火山提供了一个独特的窗口,进入最近的海洋火山活动.
研究的目的:
- 测量来自基拉韦亚的深海玄武岩中的放射性和含量.
- 评估最近海洋岩的放射测年方法的可靠性.
- 评估对海洋底扩散率计算的影响.
主要方法:
- 放射测年技术分析和同位素.
- 对玄武岩样本进行地质化学分析.
- 岩流的平流图分析.
主要成果:
- 深海玄武岩的测定年龄随样本深度的增加而增加.
- 对地质上最近的岩来说,计算的年龄达到了2200万年.
- 在预期年龄和计算年龄之间观察到显著的差异.
结论:
- 深海玄武岩的放射测年需要仔细考虑诸如深度和潜在变化的因素.
- 过多的放射性同位素的存在可能导致过度估计年龄.
- 在将来自深海玄武岩的日期应用于海洋底传播研究时,建议谨慎.
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