Changes in the Virtual Dipole Moment of the Earth’s Magnetic Field in the Phanerozoic
- Авторы: Schreider A.A.1, Ignatova A.A.1, Schreider A.A.1,2, Sazhneva A.E.1, Pugin P.Y.1,3
-
Учреждения:
- Shirshov Institute of Oceanology
- OOO Gazekonomika Scientific Research Institute
- OOO Acceleration
- Выпуск: Том 57, № 6 (2017)
- Страницы: 864-869
- Раздел: Marine Geology
- URL: https://bakhtiniada.ru/0001-4370/article/view/149578
- DOI: https://doi.org/10.1134/S0001437017050162
- ID: 149578
Цитировать
Аннотация
Data on the virtual dipole moment (VDP) is distributed nonuniformly with time, which significantly complicates qualitative and quantitative analysis of its evolution. In addition to the moving average method and median values, for the first time, a technique is presented for a quasi-uniform presentation of data (interpolation method), as well as results of calculating the evolution of the VDM by this method for the Phanerozoic.
Об авторах
A. Schreider
Shirshov Institute of Oceanology
Автор, ответственный за переписку.
Email: aschr@ocean.ru
Россия, Moscow
A. Ignatova
Shirshov Institute of Oceanology
Email: aschr@ocean.ru
Россия, Moscow
Al. Schreider
Shirshov Institute of Oceanology; OOO Gazekonomika Scientific Research Institute
Email: aschr@ocean.ru
Россия, Moscow; Moscow
A. Sazhneva
Shirshov Institute of Oceanology
Email: aschr@ocean.ru
Россия, Moscow
P. Pugin
Shirshov Institute of Oceanology; OOO Acceleration
Email: aschr@ocean.ru
Россия, Moscow; Moscow
Дополнительные файлы
