相关实验视频
Updated: Jul 22, 2026

11:59
High-speed Particle Image Velocimetry Near Surfaces
Published on: June 24, 2013
复杂的剪切波速度结构在非洲和冰岛下面的图像
Ritsema1, van Heijst HJ, Woodhouse
1Seismological Laboratory, California Institute of Technology, Pasadena, CA 91125, USA. Department of Earth Sciences, Oxford University, Oxford OX1 3PR, UK.
概括
一个地幔模型揭示了非洲下面的深度热异常,将东非裂火山活动与核心地幔边界联系起来. 冰岛 冰岛 冰岛 冰岛 冰岛
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 地球科学 地球科学 地球科学
背景情况:
- 了解地幔动态对于解释地表地质特征至关重要.
- 以前的模型还没有完全捕捉到影响火山活动的深层地幔结构的范围.
研究的目的:
- 为了建模地球地幔的三维剪切波速度变化.
- 为了调查深层地幔起源的中纪洪水玄武岩火山运动和东非的活跃裂.
主要方法:
- 开发了地幔的三维切尔波速度模型.
- 分析了地震波的传播,以推断地幔结构和热异常.
主要成果:
- 确定了一个倾斜的低速度异常,从东南大西洋下方的核心-地幔边界 (CMB) 延伸到东非下方的上层地幔.
- 这种广泛的异常表明阿法尔火山活动,东非裂和遥远的CMB热异常之间存在联系.
- 在冰岛下方发现了一个明显的低速异常,仅限于上层地幔.
结论:
- 纪洪水岩火山活动和东非裂的活跃裂可能是由CMB的深度热异常驱动的.
- 这些发现突显了深层地幔结构对大陆裂变和火山活动的重大影响.
- 与东非火山运动相比,冰岛的火山运动似乎具有较浅,独特的起源.
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