Theoretical temperature and grain-size dependence of domain state in ) = 0.6 titanomagnetite.

B. M. Moskowitz, S. L. Halgedahl

Research output: Contribution to journalArticlepeer-review

28 Scopus citations

Abstract

Domain state calculations have been made for ) = 0.6 titanomagnetite as a function of grain size, temperature, stress and exchange constant, based on the equilibrium domain models of Amar and Kittel.-from Authors

Original languageEnglish (US)
Pages (from-to)10,667-10,682
JournalJournal of Geophysical Research
Volume92
Issue numberB10
StatePublished - 1987

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