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结构控制和深度聚类在米洛斯岛的架子上广泛的热水气孔
Paraskevi Nomikou1, Konstantina Bejelou2, Andrea Koschinsky3
1Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Athens, Greece. evinom@geol.uoa.gr.
Scientific reports
|November 27, 2025
概括
研究人员在希腊米洛斯岛附近发现了一个新的中等深度的热液喷气场. 这一重大发现描述了大陆架上这些独特的地质特征的空间分布和流体特性.
科学领域:
- 地质科学 地质科学
- 海洋地质学海洋地质学
- 水热通风系统 水热通风系统
背景情况:
- 希腊的米洛斯岛架在构造学上活跃,已知有火山和热水活动.
- 与浅层或深海系统相比,中等深度的热水喷口仍未得到充分探索.
研究的目的:
- 为了全面描述米洛斯岛架上以前未经记录的中度深度热水风口场.
- 研究这些通风口的空间分布,形态和流体特性.
主要方法:
- 高分辨率的地质物理调查.
- 使用ROV MARUM-SQUID收集数据,包括化学,物理和视觉数据.
- 对活跃故障系统的通风分布的分析.
主要成果:
- 发现了一个新的中等深度热水喷气场 (30-230米),有三个主要区域:Aghia Kiriaki,Paleochori-Thiorychia和Vani.
- 风口分布显示出双模模式 (高峰在130米和180米),在一个区域内,三模集群在210米附近.
- 浅浅的通风口具有微生物和气体;更深的通风口表现出广泛的,CO2脱气烟和沸的液体 (>180°C).
结论:
- 该研究提供了米洛斯货架中介深度热水喷口的高分辨率表征.
- 双模/三模通风分布的原因需要进一步调查.
- 这些发现强调了探索中等深度的热水系统对于理解地质过程的重要性.
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