经过长时间的多次岩充电,最终引发了火山火山的喷发,埃奥利群岛的喷发
Marisa Giuffrida1, Giuseppe Salerno2, Marco Viccaro3,4
1Dipartimento di Scienze Biologiche, Geologiche e Ambientali, Università degli Studi di Catania, Corso Italia 57, Catania, Italy.
Scientific reports
|January 8, 2025
概括
在火山火山之前,深沉的岩多次补充了浅层系统.
科学领域:
- * 火山学和岩石学.
- *地质化学和地质物理学.
背景情况:
- * 1888-90年拉福萨火山喷发,提供了关于火山管道系统动态的见解.
- * 了解岩的补充对于评估火山风险至关重要.
研究的目的:
- *为了限制1888-90年火山爆发之前的水管系统重新启动的时间.
- * 调查近期脱气危机中涉及的岩起源,深度和体积.
- * 为了使石油学数据与SO2流动趋势相协调.
主要方法:
- *分析了喷发产品中的克林皮洛克森组成异质性的分析.
- *自1978年以来二氧化硫 (SO2) 流量的时间趋势分析.
- * 石油和地质化学数据与脱气记录的整合.
主要成果:
- * 在1888-90年火山爆发前的85-140,16-35和2-7年间,发生了三个不同阶段的岩岩层补充.
- * SO2数据 (1978-2024) 显示入性岩体积为~26-86 × 10^6 m^3.3 的.
- * 浅层的岩储在上个世纪被多次岩注入显著加压.
结论:
- *深层岩迁移和浅层系统沉积发生在不同的阶段.
- *最近的脱气过程中所涉及的岩体积与1888-90年的喷发相美.
- * 火山系统显示了持续的岩输入和加压的证据.
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