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Ю. В. Брусиловский
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The crustal structure of Onega-Kandalaksha paleorift identified by complex analysis of the anomalous magnetic field of the White Sea
by
A. S. Baluev
,
Yu. V. Brusilovsky
,
A. N. Ivanenko
,
А. С. Балуев
,
Ю
.
В
.
Брусиловский
,
А. Н. Иваненко
Published in
Geodynamics & Tectonophysics
(2018)
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Related Subjects
effective magnetization
field separation
inverse problem
magnetic layer model
riftogenesis
модель магнитоактивного слоя
обратная задача
разделение полей
рифтогенез
эффективная намагниченность
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