behavior of the magnetism of spinel magnetite (Fe 3 O 4) under pressure in the 0–10 GPa
range and at temperatures of 130–300 K. We find a significant but continuous decrease of
the magnetic moments at both the A and B sites to at least 10 GPa, as well as an absence of
any detectable pressure dependence of the oxygen atomic parameter. The data indicate a
very weak dependence of the saturation moment on pressure and temperature and rule out …