Magnetite is an abundant magnetic mineral that commonly records the ancient magnetic
field in a wide variety of rock types. When cooled below≈ 124 K, magnetite undergoes a …

Magnetic susceptibility behaviour around the Verwey transition of magnetite (≈ 125 K) is
known to be sensitive to stress, composition and oxidation. From the isotropic point (≈ 130 …

We studied the effects of stress on the Verwey transition for pure, stoichiometric, synthetic
multidomain magnetite and for natural multidomain magnetite having both relatively low and …

Experimental results on the change in the Verwey transition temperature in magnetite under
compression exhibit puzzling variability, with slopes ranging from− 6 to+ 16K/GPa. Our …

To elucidate mechanisms controlling the magnetic properties of multidomain magnetite
below the Verwey transition, we have conducted magnetization measurements between 5 …

We have conducted the first in‐situthermal demagnetization experiments on low‐
temperature remanences of magnetite under high pressure up to 0.7 GPa, to investigate the …

Hysteresis loops have been measured as a function of temperature between 10 K and room
temperature for two size fractions of crushed magnetite: 1–5 μm (pseudo-single-domain …

There is a general agreement, that magnesium silicate perovskite (Pv) comprises around 80
vol% of the Earth's lower-mantle, making it by volume the most abundant mineral in our …

The magnetic properties of magnetite (Fe3O4) are strongly dependent on the internal stress
related to stress-controlled regions and to closure domains associated with defects. The …

The magnetic behaviour of magnetite at low temperatures is dominated by its transformation
to a monoclinic crystal structure that is simultaneously ferrimagnetic, ferroelastic and …