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一个组成的临界点,控制着岩石岩的动员和喷发风格
D Di Genova1,2, S Kolzenburg2, S Wiesmaier2
1School of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol BS8 1RJ, UK.
岩石的组成决定了火山喷发的风格. 微妙的组成变化会导致显著的粘度变化,影响喷发是否充或爆炸,影响全球气候.
科学领域:
- 地质化学
- 火山学
- 材料科学
背景情况:
- 大规模的爆炸性喷发影响全球气候,
- 岩以水丰富的间隙溶液的形式存储,但动员机制尚不清楚.
- 石灰岩喷发的原因尚未完全理解.
研究的目的:
- 在黄石火山系统的组成范围内研究石灰岩融化的粘度变化.
- 确定控制融和喷发行为的组成转折点.
- 了解融化结构在火山过程中的作用.
主要方法:
- 石溶液的粘度测量
- 通过拉曼光谱检测确认融结构的重组.
- 用热力学建模来探索融物质的组成影响.
主要成果:
- 一个狭窄的组成区域显示粘度增加了多达两个数量级.
- 粘度变化与融化结构重组有关,目前的模型没有预测.
- 一个关键的组成转折点将全球的喷发性和爆炸性沉积物分开.
结论:
- 石融化成分对动员和喷发动态具有决定性作用.
- 不仅是水或水晶含量, 控制喷发风格.
- 这些发现有助于更好地了解大型火山系统的行为和气候影响.
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