概括
深海地震调查揭示了海洋地下以前隐藏的7.3公里/秒的速度层. 这一在马歇尔群岛和夏威夷群岛之间发现的发现可能在全球范围内广泛传播.
科学领域:
- 地质物理学 地质物理学
- 海洋学 海洋学 海洋学
- 地震学 地震学
背景情况:
- 海洋地和上层地幔的地震结构是理解板块构造学的关键.
- 之前的折射研究已经确定了海洋地内不同的层.
研究的目的:
- 为了研究深海底的地震速度结构.
- 为了识别和描述海洋地和地幔之间的潜在地震层.
主要方法:
- 在马歇尔群岛和夏威夷群岛之间进行了深海折射测量.
- 使用连续气炮地震折射数据,揭示了微妙的速度层.
主要成果:
- 确定了一个独特的地震层,其速度为7.3公里/秒.
- 这层位于海洋地 (6.8公里/秒) 和地幔之间.
- 该层以前被掩盖为次级地震到达.
结论:
- 一个以前未知的地震层存在于海洋地下,在海洋深处.
- 这层可能是广泛分布的深海盆地的共同特征.
- 需要进一步的研究来确定这个层的组成和范围.
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