The composition and magnetic properties of foraminifers from bottom sediments of the Mid-Atlantic Ridge and their artificial analogs obtained by hydrothermal synthesis were studied. The presence of magnetic hysteresis and theoretical modeling of hysteresis characteristics made it possible to assume the presence
of grains of nonstoichiometric magnetite in single- and few-domain states.
Original languageEnglish
Pages (from-to)523-530
Number of pages8
JournalBulletin of the Russian Academy of Sciences: Physics
Issue number4
StatePublished - 1 Apr 2024

    Research areas

  • ferrimagnet, foraminifera, hydrothermal synthesis, iron oxide, magnetic granulometry, magnetic hysteresis, magnetic state, magnetite, theoretical modeling

ID: 118492610