地球地中的化学分化,冷藏和重新调动岩
M D Jackson1, J Blundy2, R S J Sparks2
1Department of Earth Science and Engineering, Imperial College London, London, UK. m.d.jackson@imperial.ac.uk.
Nature
|December 5, 2018
概括
岩池中的反应性融流解释了分化岩的形成和较古老的晶体的储存. 这一过程挑战了火山地质学和火山学中的传统岩模型.
科学领域:
- 岩石地质
- 火山学
- 地质化学
背景情况:
- 传统的地岩模型依赖于高融率的'岩室'范式.
- 最近的数据表明,岩存储在低化率的"池"中,这是一个有间隙化的多孔晶体框架.
- 现有的模型无法解释地岩的几个常见特征.
研究的目的:
- 调查地中反应性融流的作用.
- 解释化学差异化的岩的产生和旧的晶体的储存.
- 提出一种新的岩存储和分化模式.
主要方法:
- 在池中分析反应性融流动.
- 模拟化和晶体化反应.
- 模型生成的微量元素形状与自然实例的比较.
主要成果:
- 反应性融流,由浮性融透驱动,是池中的一个关键过程.
- 这种过程产生了低晶度,化学分化的岩,可以升起或爆发.
- 反应性流解释了分化的岩中较古的水晶的存在和岩组成的双态性.
结论:
- 的储存和分化主要通过长寿命储存器的反应性流发生.
- 这挑战了长期存在的岩室的分量结晶模型.
- 反应性融流为观察到的岩特征提供了更全面的解释.
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