地震动力学. 地震动力学. 从诱导的地地震速度下降到加压的火山流体进行映射
F Brenguier1, M Campillo2, T Takeda3
1Institut des Sciences de la Terre, Université Joseph Fourier, CNRS, F-38041 Grenoble, France. florent.brenguier@ujf-grenoble.fr.
概括
火山爆发源于深层流体的压力. 科学家们现在可以通过测量地震速度在压力下如何变化来绘制这些压力高的火山区域的图像,从而揭示火山系统的特征.
科学领域:
- 地质物理学 地质物理学
- 火山学 火山学是一门学科.
- 地震学 地震学
背景情况:
- 火山喷发是由深层热火山流体释放的压力驱动的.
- 了解受压流体影响地区的范围对于火山危险评估至关重要.
研究的目的:
- 为了展示一种用于成像压缩火山区域的新方法.
- 为了研究地震速度变化和地压力扰动之间的关系.
主要方法:
- 利用了来自日本Hi-net地震网络的地震噪声记录.
- 测量了2011年东北奥基地震后火山区的地地震速度变化.
- 解释地震速度的减小是由于动态应力导致的机械减弱的指标.
主要成果:
- 在火山区域以下观察到显著的co-seismic地地震速度减少.
- 将这些减少与地震波诱导的动态应力对压缩地的机械削弱联系起来.
- 证明了地震速度变化与应力扰动相关.
结论:
- 地图化地震速度对动态应力扰动的易感性,为绘制火山系统的图像提供了一种新的方式.
- 这种技术可以帮助描述和监测火山活动.
- 提供了关于火山地下结构和火山机械状况的见解.
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