冰岛Bárðarbunga扩散中心沿线最近的Holuhraun喷发的现有结构控制
Arne Døssing1, Mick Emil Kolster2, Eduardo L S da Silva3,2
1Crustal Magnetometry Technology & Research Group (CMAGTRES), Division of Geomagnetism & Geospace, DTU Space, Centrifugevej 356, 2850 Kgs., Lyngby, Denmark. ards@space.dtu.dk.
Scientific reports
|February 9, 2024
概括
高分辨率的无人机磁性调查揭示了冰岛隐藏的断层结构. 这些以前未知的断层影响了霍鲁哈伦主要的火山爆发,为裂区地力学提供了新的见解.
科学领域:
- 地质物理学 地质物理学
- 构造学 构造学 构造学 构造学
- 火山学 火山学是一门学科.
背景情况:
- 冰岛的裂区提供了对不同板块边界的洞察力.
- 传统的地质物理方法往往错过了更老的,埋藏的结构控制活跃的地力学.
- 现有的气磁数据仅限于大规模的区域研究.
研究的目的:
- 通过使用高分辨率无人机磁场来调查冰岛裂区域的结构复杂性.
- 识别活跃和被动结构,包括那些被火山沉积埋藏的结构.
- 了解预先存在的结构对火山事件的控制.
主要方法:
- 无人机拖的磁性标量场和标量梯度测量调查.
- 在Bárðarbunga传播中心采集高分辨率的气磁数据.
- 对地下磁化对比的分析.
主要成果:
- 密集间隔,并联和斜断层的详细地图.
- 发现了一个重要的,以前未知的东北倾斜断层结构.
- 鉴定断层与霍鲁拉恩火山爆发地点的巧合.
结论:
- 无人机磁力为裂区域研究提供了前所未有的空间分辨率.
- 新发现的断层可能控制了1797年和2014-15年霍卢拉恩喷发期间的岩迁移.
- 预先存在的结构在控制冰岛裂区域的火山活动方面发挥着至关重要的作用.
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