概括
中大西洋山脊岩石的同位素分析显示了和的变化. 放射性同位素的这些差异表明地球上的区域化学异质性.
科学领域:
- 地质化学 地质化学
- 同位素地质学的同位素.
- 石化学 石化学是一门学科.
背景情况:
- 中大西洋山脊是理解地幔过程的关键区域.
- 像和这样的元素的同位素组成可以追踪地幔源的变化.
- 之前的研究表明海洋地幔来源的异质性.
研究的目的:
- 为了确定来自两个中大西洋山脊岛屿的岩石样本中的和的同位素组成.
- 为了研究放射性同位素的岛内和岛内变化.
- 评估这些变异对理解上层地幔异质性的影响.
主要方法:
- 在岩石样本中确定和的同位素组成.
- 对-206/-204 (Pb-206/Pb-204) 和-208/-204 (Pb-208/Pb-204) 的比例进行分析.
- 对同位素比率的分析.
主要成果:
- 观察到和的放射性同位素在岛内和岛内有显著的变化.
- 来自阿森森岛的玄武岩显示,与Gough岛 (18.4) 相比,Pb-206/Pb-204比率 (19.5) 更高.
- 两个岛屿的气管体呈现出比各自的玄武岩更多的放射性和.
结论:
- 岛际同位素组成的差异表明,上层地幔的-和-比率存在区域差异.
- 同位素组成作为一个有价值的工具,用于调查地球地幔内的化学异质性.
- 这些发现凸显了大西洋中部山脊下方地幔源的复杂性质.
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