在夏威夷海底的岩石网
John D Wilding1, Weiqiang Zhu1, Zachary E Ross1
1Seismological Laboratory, California Institute of Technology, Pasadena, CA, USA.
概括
科学家使用先进的地震监测发现了夏威夷的深层岩系统. 这种地幔的复杂性起到了关键的作用,将深层岩源与Kīlauea和Mauna Loa等火山联系起来.
科学领域:
- 地质学
- 火山学
- 地震学
背景情况:
- 了解深层岩运输是解读夏威夷火山系统动态的关键.
- 2018年Kīlauea火山崩之前,地幔地震活动显著增加.
研究的目的:
- 在夏威夷火山系统下的深层岩层结构的图像和特征.
- 调查地幔地震与火山管道之间的联系.
主要方法:
- 使用先进的地震监测技术.
- 应用深度学习算法来分析大量的地震数据集 (近20万个事件).
- 测绘地震活动以了解决地下结构.
主要成果:
- 在深度36-43公里处发现15公里长的近水平.
- 发现一个25公里长的地震带连接到Kīlauea的更深的管道.
- 观测到一个地震柱连接到边缘复杂的浅处脱落附近的毛纳洛阿.
结论:
- 作为一个关键的连接点,
- 在夏威夷火山系统中展示了广泛的岩石连接.
- 突出了深度学习在地震成像中对理解火山结构的有用性.
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