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从210Pb-226Ra-230Th不平衡的海洋岩的最低速度限制
K H Rubin1, I van der Zander, M C Smith
1Department of Geology and Geophysics, Hawaii Center for Volcanology, University of Hawaii, 1680 East-West Road, Honolulu, Hawaii 96822, USA. krubin@hawaii.edu
Nature
|September 24, 2005
概括
中洋山脊的岩石化可以迅速发生,地幔融化物被运输,积累,并在几十年内爆发. 这种快速的过程影响了地结构和山脊火山的热水活动.
科学领域:
- 地质化学 地质化学
- 火山学 火山学是一门学科.
- 放射地质化学 放射地质化学
背景情况:
- 海洋中部山脊占全球地岩的70% .
- 了解岩输入时间尺度对于地结构,热水活动和生物圈动态至关重要.
- 放射性衰变链核酸可以通过父女不平衡来评估岩时间尺度.
研究的目的:
- 为了研究中洋山脊上的岩输入的节奏.
- 用放射性不平衡来推断融化运输,积累和喷发时间表.
- 为了理解山脊火山快速岩波动的含义.
主要方法:
- 在年轻的海洋玄武岩 (<20岁) 中分析210Pb-226Ra-230Th放射性不平衡.
- 对地质化学属性的检查,包括兼容的微量元素比率.
- 应用地幔融化模型来模拟观察到的不平衡.
主要成果:
- 在中海基岩中观察到210Pb缺陷 (高达15%) 与226Ra相比,表明最近的分成.
- 最大的210Pb缺陷与富含的岩相关.
- 地化学数据排除了地-岩分化或脱气作为观察到的不平衡的主要原因.
结论:
- 地幔融化物可以被运输,积累,并在几十年内在中洋山脊上爆发.
- 在山脊火山的岩条件可以迅速波动.
- 快速融化运输机制是必要的,以保持地幔衍生的放射性不平衡.
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