概括
来自太平洋 - 南极山脊的磁异常证实了海底扩散模式,并揭示了地磁场逆转的详细历史. 这项研究估计了海洋底的扩散速度,并提供了对地球的洞察力.
科学领域:
- 地质物理学 地质物理学
- 海洋磁力学 海洋磁力学
- 板块构造学是一种板块构造学.
背景情况:
- 了解与中洋山脊相关的磁异常的产生对于破译地球历史至关重要.
- 维恩和马修斯假设为解释这些磁模式提供了一个框架.
研究的目的:
- 分析沿太平洋-南极山脊的磁异常,以支持Vine和Matthews假设.
- 为了确定海洋底的扩散速度和重建地磁场逆转.
主要方法:
- 获取和分析横跨太平洋-南极山脊的四个磁形.
- 观察到的磁异常与已知的地磁场逆转的相关性.
- 对磁性异常模式的建模以推断扩散率.
主要成果:
- 磁性异常呈现出与太平洋 - 南极山脊轴平行和对称的趋势.
- 磁体的分布和几何形状支持了Vine和Matthews的假设.
- 在过去的340万年里,海洋底的扩散速度为每年4.5厘米.
- 确定了过去10亿年地磁场逆转的详细历史.
结论:
- 这项研究使用来自太平洋-南极山脊的数据验证了Vine和Matthews假设.
- 由此得出的地磁逆转历史与在雷克扬斯山脊观察到的异常相一致,假设每年1厘米的传播速度.
- 这项研究完善了我们对海底传播动态和古磁场的理解.
相关概念视频
Magnetic Declination
Magnetic declination is the angle between true north, which aligns with the Earth's rotational axis, and magnetic north, which follows the direction of the Earth's magnetic field. This discrepancy exists because the magnetic poles do not coincide with the geographic poles. The value of magnetic declination depends on the observer's location on Earth and is subject to changes over time due to the dynamic nature of the Earth's magnetic field.The declination is called eastern when magnetic north...
Magnetic Field Lines
The representation of magnetic fields by magnetic field lines is very useful in visualizing the strength and direction of the magnetic field. Each of the magnetic field lines forms a closed loop. The field lines emerge from the north pole (N), loop around to the south pole (S), and continue through the bar magnet back to the north pole.
Magnetic field lines follow several hard-and-fast rules:
Magnetic field lines follow several hard-and-fast rules:
Magnetic Fields
A moving charge or a current creates a magnetic field in the surrounding space, in addition to its electric field. The magnetic field exerts a force on any other moving charge or current that is present in the field. Like an electric field, the magnetic field is also a vector field. At any position, the direction of the magnetic field is defined as the direction in which the north pole of a compass needle points.
A magnetic field is defined by the force that a charged particle experiences...
A magnetic field is defined by the force that a charged particle experiences...
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...
Magnetism
Magnets are commonly found in everyday objects, such as toys, hangers, elevators, doorbells, and computer devices. Experimentation on these magnets shows that all magnets have two poles: one is labeled north (N) and the other south (S). Magnetic poles repel if they are alike and attract if unlike. Moreover, both poles of a magnet attract unmagnetized pieces of iron.
An individual magnetic pole cannot be isolated. No matter how small, every piece of a magnet contains a north pole and a south...
An individual magnetic pole cannot be isolated. No matter how small, every piece of a magnet contains a north pole and a south...
Magnetic Susceptibility and Permeability
In linear magnetic materials, like paramagnets and diamagnets, magnetization is proportional to the magnetic field intensity. The constant of proportionality, a dimensionless number, is called magnetic susceptibility. The value of the susceptibility depends on the type of material.
When diamagnetic materials are placed under an external magnetic field, the moments opposite to the field are induced. Hence, the susceptibility for diamagnets has a minimal negative value of 10-5–10-6. Since...
When diamagnetic materials are placed under an external magnetic field, the moments opposite to the field are induced. Hence, the susceptibility for diamagnets has a minimal negative value of 10-5–10-6. Since...

