"inversion" of ternary equilibrium system and Earth's magnetic field
| Main Author: | 杨林 |
|---|---|
| Format: | Article Journal |
| Terbitan: |
, 2021
|
| Subjects: | |
| Online Access: |
https://zenodo.org/record/5016737 |
Daftar Isi:
- Geomagnetic inversion refers to the alternating phenomenon of the earth's magnetism pole, or geomagnetic reversal. It refers to the 180 change in the direction of the earth's magnetic field, or the polarity of the geomagnetic poles. The results of paleogeomagnetic research confirm that the polarity of the Earth's magnetic field has been reversed many times. The inversion of the geomagnetic field was initially found in residual magnetic measurements of the rock. In explaining this phenomenon, it was proposed that rock magnetization is directed opposite to the direction of modern geomagnetic field, possibly due to the rock formation direction opposite to the direction of modern geomagnetic field. For this view could not be affirmed at the time. So, it was once called the geomagnetic field inversion hypothesis. However, according to the conclusion of the law of ternary balance, the celestial body produces the corresponding magnetic field relative to the absolute stationary space movement, and the earth's rotation of the earth is this kind of spatial movement relative to the absolute static, so it will inevitably produce a magnetic field perpendicular to the direction of motion. Through this theoretical analysis, it is roughly concluded that the reversal of the earth's magnetic field generated from rotation is absolutely impossible. But why do some scientists find that the direction of rock magnetization is the opposite direction of the modern magnenetic field? In fact, this phenomenon is not formed after the reversal of the earth 's magnetic pole, but after the earth' s magnetic pole offset. (The English version is converted by translation software, so there may be many translation errors.The English version is converted by translation software, so there may be many translation errors.)