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太平洋地区的非偶极子磁场微弱是地磁场长期变化所致,这一现象可用本人曾提出的非偶极子磁场模型较好地进行解释,而不是所谓地幔深部的高导层屏敝的结果。在这一地区地壳磁异常亦很微弱。在地质构造上还有其他方面的特征。因而说明太平洋撞击成因的假说是有一定的道理。
The weakness of the non-dipole magnetic field in the Pacific is due to the long-term changes in the geomagnetic field. This phenomenon can be well explained by the non-dipole magnetic field model I proposed earlier rather than the so-called high-conductivity screen mask in the deep mantle . Crustal magnetic anomalies are also very weak in this area. In the geological structure there are other aspects of the characteristics. Therefore, the hypothesis of the origin of the Pacific Ocean collision has some truth.