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在玛约特岛下面,有丰富化的岩石储存库的磁体证据
Pierre Wawrzyniak1, Fabrice Gaillard2, Sophie Hautot3
1BRGM, Bureau des Recherches Géologiques et Minières, Orléans, France. P.Wawrzyniak@brgm.fr.
Nature
|October 30, 2025
概括
研究人员在马约特岛下方拍摄了一座巨大的岩石库, 这一发现挑战了岩模型,
科学领域:
- 地质学
- 火山学
- 石油学
背景情况:
- 由于无法直接取样,人们对地岩库的构成了解甚少.
- 当前的跨地岩系统 (TCMS) 模型假定水库主要是结晶型 ("岩") 且化程度最小.
- 这种TCMS模型主要基于间接的地质物理证据和从喷发材料中得到的有限的融化分数估计.
研究的目的:
- 在马约特岛下面描绘和描述一个潜在的岩石储存库.
- 为了确定这个水库中的融化分数.
- 评估对理解地岩储存和火山过程的影响.
主要方法:
- 电阻成像被用来检测地下结构.
- 实验室测量了梅奥特岛的火山环境中的导率.
- 喷发产品的地化学和纹理分析被用于比较.
主要成果:
- 在海平面以下23±1公里处成像了一个显著的电导体,被解释为岩层储存库.
- 这座水库很大 (超过200立方公里),融化率很高 (22-42%).
- 这种融化分数与迈奥特岛喷发的融化分化模型一致,可能与最近的海底喷发有关.
结论:
- 图像中的水库具有高含量,挑战了TCMS中的"岩"主导地位.
- 这一发现直接证实了地中大量融的岩.
- 这些发现为迈奥特最近火山活动的水管系统提供了关键的见解.
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