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