美国圣海伦斯山火山活动的地质化学前体
Kim Berlo1, Jon Blundy, Simon Turner
1Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Rd, Bristol BS8 1RJ, United Kingdom. Kim.Berlo@bristol.ac.uk
概括
在圣赫伦斯山喷发之前的脱气和结晶过程影响了喷发风格. 岩中的地化学特征显示了几十年到几天的脱气,表明岩停滞和挥发性积累.
科学领域:
- 火山学 火山学是一门学科.
- 地质化学 地质化学
背景情况:
- 岩脱气和结晶之间的相互作用对于理解火山爆发至关重要.
- 之前的研究确定了这些过程对1980年圣海伦斯火山爆发的意义.
研究的目的:
- 调查火山爆发前岩脱气的时间和特征.
- 使用地化学数据,将脱气模式与喷发风格相关联.
主要方法:
- 对微量元素,特别是的分析.
- 测量短寿命放射性同位素,包括-210和-226.
- 解释岩内地化学特征的解释.
主要成果:
- 脱气发生在较长的时间内,从几十年到火山爆发前几天.
- 地化学特征表明,岩在火山管道内停滞不前.
- 这种停滞导致挥发性积累和-210过剩的形成,标志着深度脱气.
结论:
- 脱气模式表明圣赫伦斯山的喷发风格.
- 岩停滞和挥发性积累是喷发前的关键过程.
- 过剩的210作为地质化学标记物,用于消气岩.
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