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 language | English (US) |
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Pages (from-to) | 10,667-10,682 |
Journal | Journal of Geophysical Research |
Volume | 92 |
Issue number | B10 |
State | Published - 1987 |