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Evolution of the Virtual Dipole Moment in Earth's Geological History

机译:地球地质史上虚拟偶极矩的演变

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Data of the International Bank of Digital Information on the time distribution of the virtual dipole moment (VDM), supplemented by data of more recent studies (a total of 5645 values), were used as the basis for analyzing the distribution of VDM values for Earth's history using the concept of the Earth's magnetic dipole field. The VDM behavior is characterized by a positive linear trend from 4.2 x 10 (22) Am-2 (4.2 GA ago) to 5.15 x 10(22) Am-2 today. Against a linear increase in the field, VDM undulations nonuniformly distributed over time have been recorded, varying in magnitude from 1.7 to 3.7 x 10(22) Am-2 wavelength from 220 to 920 Ma. The average wavelength of such undulations is estimated at 570 Ma, which in order of magnitude approaches the period of the Wilson cycle. It has been revealed for the first time that the magnitudes of magnetic field undulations over time are oscillatory in nature and increase toward present day.
机译:关于虚拟偶极矩(VDM)的时间分布的国际数据库数据库,补充说,通过更新的研究(总共5645个值)作为分析地球的VDM值分布的基础 历史使用地球磁偶极场的概念。 VDM行为的特点是从4.2 x 10(22)AM-2(4.2毛之前)的正线性趋势为今天至5.15 x 10(22)AM-2。 在该领域的线性增加,VDM波浪不均匀地分布在时间上,从220到920 mA的1.7到3.7×10(22)am-2波长幅度不同。 这种起伏的平均波长估计为570 mA,其幅度为威尔逊周期的时期。 首次揭示了第一时间,磁场起伏随时间随着时间的推移的大小是自然的振荡,并且朝向现今的增加。

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