夏威夷羽毛的年轻来源.
Alexander V Sobolev1, Albrecht W Hofmann, Klaus Peter Jochum
1ISTerre, University Joseph Fourier, Grenoble 1 and CNRS, BP 53, 38041 Grenoble, France. alexander.sobolev@ujf-grenoble.fr
Nature
|August 12, 2011
概括
海洋岛屿的火山活动涉及到海洋地的回收. 来自夏威夷岩的新同位素数据揭示了海水污染,这表明地幔循环速度比以前估计的要快.
科学领域:
- 地质化学 地质化学
- 同位素地球化学 同位素地球化学
- 地幔石化学地幔石化学
背景情况:
- 海洋岛屿的火山活动是由海洋地通过沉降和地幔羽毛的循环回收来解释的.
- 这种回收的年代对于理解地幔循环率至关重要.
- 以前使用和Re-Os同位素的测年方法由于混合和的移动性而存在局限性.
研究的目的:
- 为了研究在地幔羽毛中海洋地回收的时间尺度.
- 为了确定导致夏威夷火山活动的沉积海洋地的年龄.
- 为了精确地估计地幔循环速率.
主要方法:
- 分析了来自毛纳洛阿橄烯晶体的138个融的-87/-86 ((87) Sr/(86) Sr) 比率.
- 与海水和古代地签名的同位素组成的比较.
- 对同位素数据的建模以推断源污染和年龄.
主要成果:
- 在Mauna Loa的岩中发现了巨大的地幔源异质性.
- 耗尽的融含量中的高放射性与2亿至6亿5千万年前的海水相匹配.
- 这表明在沉降之前,毛纳洛阿源岩的海水污染.
结论:
- 海水污染为沉降的海洋地提供了一个"时间".
- 2亿至6亿年前的海洋地的存在意味着地幔的循环速度更快.
- 平均地幔循环速率估计约为每年2 (±1) 厘米,比以前认为的要快.
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