源水库控制大规模火山喷发的规模,频率和组成
Catherine A Booth1, Matthew D Jackson1, R Stephen J Sparks2
1Department of Earth Science and Engineering, Imperial College London, London, UK.
Science advances
|May 10, 2024
概括
大规模的火山喷发是由深层水库中的浮力岩积累驱动的. 这个过程解释了喷发的大小,频率,以及为什么地球没有经历更大的状喷发.
科学领域:
- 地质科学 地质科学
- 火山学 火山学是一门学科.
- 岩动力学 岩动力学
背景情况:
- 大规模的爆炸性火山喷发构成重大自然危险.
- 了解控制喷发规模和频率的机制对于危险评估至关重要.
研究的目的:
- 解释大规模爆炸性火山喷发的规模,频率和组成.
- 确定控制岩积累和从源水库转移到次火山腔的关键过程.
主要方法:
- 在长寿,高晶度的岩储层中模拟融透过程.
- 对岩积累,浮力驱动的上升和断裂传播的分析.
主要成果:
- 性岩积聚在深层水库中的低晶度层中,通过融的透.
- 浮力,而不是结晶性,控制着磁石通过磁石驱动的断裂,偶尔将磁石转移到亚火山腔中.
- 确定了最大的岩喷发的最佳水库大小,与自然系统相一致.
结论:
- 拟议的模型解释了大型状喷发的观测特征.
- 浮力是来自深层水库的岩输送的主要驱动力.
- 该模型为了解地球上的喷发规模的极限提供了一个框架.
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