Evolution of the Virtual Dipole Moment in Earth’s Geological History
- Авторлар: Schreider A.A.1, Sazhneva A.E.1, Varga P.2, Denis C.3
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Мекемелер:
- Shirshov Institute of Oceanology, Russian Academy of Sciences
- Seismological Observatory, Geodetic, and Geophysical Institute, Hungarian Academy of Sciences
- Institute of Astrophysics at Liege University
- Шығарылым: Том 59, № 5 (2019)
- Беттер: 771-776
- Бөлім: Marine Geology
- URL: https://journals.rcsi.science/0001-4370/article/view/149939
- DOI: https://doi.org/10.1134/S0001437019050187
- ID: 149939
Дәйексөз келтіру
Аннотация
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 × 10 22 Am2 (4.2 GA ago) to 5.15 × 1022 Am2 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 × 1022 Am2 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.
Негізгі сөздер
Авторлар туралы
A. Schreider
Shirshov Institute of Oceanology, Russian Academy of Sciences
Хат алмасуға жауапты Автор.
Email: aschr@ocean.ru
Ресей, Moscow, 117218
A. Sazhneva
Shirshov Institute of Oceanology, Russian Academy of Sciences
Email: aschr@ocean.ru
Ресей, Moscow, 117218
P. Varga
Seismological Observatory, Geodetic, and Geophysical Institute, Hungarian Academy of Sciences
Email: aschr@ocean.ru
Венгрия, Budapest
C. Denis
Institute of Astrophysics at Liege University
Email: aschr@ocean.ru
Бельгия, Liege
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