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确定海洋石化层-石化层系统的内在衰减
Nozomu Takeuchi1, Hitoshi Kawakatsu1, Hajime Shiobara1
1Earthquake Research Institute, The University of Tokyo, Yayoi 1-1-1, Bunkyo-ku, Tokyo 1130032, Japan.
概括
地震波分析揭示了海洋石化层-石化层系统 (LAS) 中明显的频率依赖衰减. 这种差异突出了独特的热力学特性和散射机制,使得天气层与石化层有所区别.
科学领域:
- 地质学
- 地震学
- 地球科学
背景情况:
- 海洋石化层-石化层系统 (LAS) 对于理解板块构造学至关重要.
- 描述LAS的热力学特性是必不可少的,但具有挑战性.
- 地震波减弱提供了一个强大的工具来探测这些特性.
研究的目的:
- 量化分离内在 (无弹性) 和外在 (散射) 地震波衰减.
- 为了推断海洋LAS的热力学特性.
- 了解石化层与石化层之间的波浪传播差异.
主要方法:
- 使用宽带海底地震计记录P和S地震波.
- 通过海洋石化层-石化层系统分析地震波传播.
- 从数量上分离内在和外在的减弱效应.
主要成果:
- 在更高的频率 (~3 Hz) 中观察到强烈的内在衰减.
- 发现了无频无弹性, 与低频表面波数据一致.
- 在石化层中确定了依赖频率的内在衰减.
- 实验室观察到的广泛峰值消散是天气层的特征.
结论:
- 石化层表现出频率独立的无弹性,而石化层表现出频率依赖的衰减.
- 这种频率依赖的差异为天气层和岩层的不同热力学特性和散射机制提供了新的见解.
- 这项研究阐明了实验室观察到的海洋气体消散的作用.
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