在夏威夷热点下面的地幔剪切波速度结构
Cecily J Wolfe1, Sean C Solomon, Gabi Laske
1Hawaii Institute of Geophysics and Planetology, University of Hawaii at Manoa, Honolulu, HI 96822, USA. cecily@soest.hawaii.edu
概括
地震成像显示,在夏威夷热点下面有一个深层地幔羽毛. 这种高温的上升源于下层地幔,影响了岛链的结构.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 地幔动力学地幔动力学
背景情况:
- 了解海洋热点下的地幔结构对于确定它们的起源深度至关重要.
- 夏威夷群岛是火山热点的一个典型例子.
研究的目的:
- 为了定义夏威夷群岛下方的三维地幔结构.
- 为了调查夏威夷热点的热异常的深度和范围.
主要方法:
- 使用海底和陆地地震计网络获取地震剪切波速度数据.
- 整合SKS (剪切波分裂) 观测,以将地震分辨率扩展到更深处.
主要成果:
- 一个沿着夏威夷岛屿链延长的上层地幔低速异常的识别.
- 观测周围的抛物线高速异常.
- 证实了延伸到地幔过渡区 (410660公里深度) 的低速度,与稀薄相一致.
- 在夏威夷下面和东南部探测到一个宽的低速度区域,深度为1500公里.
结论:
- 地震图像强烈表明,夏威夷热点是由从下层地幔上升的高温羽毛推动的.
- 观察到的结构为夏威夷热点的深层起源提供了证据.
相关概念视频
Shock Waves
While deriving the Doppler formula for the observed frequency of a sound wave, it is assumed that the speed of sound in the medium is greater than the source's speed through it. When this condition is breached, a shock wave occurs.
When the source's speed approaches the speed of sound, constructive interference between successive wavefronts emitted by the source occurs immediately behind it. Initially, scientists believed that this constructive interference would result in such high pressures...
When the source's speed approaches the speed of sound, constructive interference between successive wavefronts emitted by the source occurs immediately behind it. Initially, scientists believed that this constructive interference would result in such high pressures...
Elastic Strain Energy for Shearing Stresses
As discussed in previous lessons, strain energy in a material is the energy stored when it is elastically deformed, a concept crucial in materials science and mechanical engineering. This energy results from the internal work done against the cohesive forces within the material. When a material undergoes shearing stress and corresponding shearing strain, the strain energy density, which is the energy stored per unit volume, is calculated. Within the elastic limit, where the stress is...
Magnetostatic Boundary Conditions
An electric field suffers a discontinuity at a surface charge. Similarly, a magnetic field is discontinuous at a surface current. The perpendicular component of a magnetic field is continuous across the interface of two magnetic mediums. In contrast, its parallel component, perpendicular to the current, is discontinuous by the amount equal to the product of the vacuum permeability and the surface current. Like the scalar potential in electrostatics, the vector potential is also continuous...
Speed of a Transverse Wave
The speed of a wave depends on the characteristics of the medium. For example, in the case of a guitar, the strings vibrate to produce the sound. The speed of the waves on the strings and the wavelength determine the frequency of the sound produced. The strings on a guitar have different thicknesses but may be made of similar material. They have different linear densities, and the linear density is defined as the mass per length.
One of the key properties of any wave is the wave speed. Light...
One of the key properties of any wave is the wave speed. Light...
Travelling Waves
A wave is a disturbance that propagates from its source, repeating itself periodically, and is typically associated with simple harmonic motion. Mechanical waves are governed by Newton's laws and require a medium to travel. A medium is a substance in which a mechanical wave propagates, and the medium produces an elastic restoring force when it is deformed.
Water waves, sound waves, and seismic waves are some examples of mechanical waves. For water waves, the wave propagation medium is water;...
Water waves, sound waves, and seismic waves are some examples of mechanical waves. For water waves, the wave propagation medium is water;...
Propagation of Waves
When a wave propagates from one medium to another, part of it may get reflected in the first medium, and part of it may get transmitted to the second medium. In such a case, the interface of the two mediums can be considered as a boundary that is neither fixed nor free.
Consider a scenario where a wave propagates from a string of low linear mass density to a string of high linear mass density. In such a case, the reflected wave is out of phase with respect to the incident wave, however the...
Consider a scenario where a wave propagates from a string of low linear mass density to a string of high linear mass density. In such a case, the reflected wave is out of phase with respect to the incident wave, however the...


