爆炸性火山活动可能不是岩碎片化的必然后果
Helge M Gonnermann1, Michael Manga
1Earth and Planetary Science, University of California, Berkeley, California 94720, USA. hmg@seismo.berkeley.edu
Nature
|December 4, 2003
概括
岩碎片,爆炸性喷发的关键,也可以发生非爆炸性. 这一过程有助于岩的脱气,有可能防止暴力的火山爆发,并挑战对爆炸性火山的传统观点.
科学领域:
- 火山学 火山学是一门学科.
- 地质物理学 地质物理学
- 材料科学 是一种材料科学.
背景情况:
- 爆炸性火山喷发的特点是由于气泡膨胀和粘性应力而导致的岩碎片.
- 爆炸性和喷发性喷发之间的过渡动态,尽管具有相似的岩挥发性含量,但仍然不太了解.
- 喷射岩的脱气量明显高于爆炸性喷发的岩.
研究的目的:
- 为了研究控制火山爆发风格的碎片化机制.
- 探索岩脱气在喷发性和爆炸性喷发之间的过渡过程中的作用.
- 挑战传统观点,即岩碎片化不可避免地导致爆炸性火山活动.
主要方法:
- 分析泡生长和岩流动期间的粘性应力.
- 在火山管道壁附近的碎片化过程的建模.
- 间歇性透断裂网络生成的观察.
主要成果:
- 粘性剪切碎片发生在流和爆炸性喷发场景中.
- 在管道壁附近的非爆炸性碎片化可以产生透的断裂网络.
- 这种碎片化机制被认为是岩脱气的重要因素.
结论:
- 粘性剪切的岩碎片化可以发生而不会导致爆炸性喷发.
- 非爆炸性碎片化在上升期间的岩脱气中起着至关重要的作用.
- 这些发现表明,爆炸性火山活动并不是岩碎片化不可避免的结果.
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