Natural materials contain small grains of magnetic iron oxides that can record information
about the magnetic field of the Earth when they form and can be used to document changes …

Fine particles of titanomagnetites (Fe3‐xTixO4, x> 0.5) in the pseudo‐single‐domain (PSD)
size (0.5–20 μm) are important carriers of natural remanent magnetization in basalts …

The minerals carrying the magnetic remanence in geological samples are commonly a solid
solution series of iron‐titanium spinels known as titanomagnetites. Despite the range of …

Abstract Domain observations using Bitter patterns have been made on x= 0.6
titanomagnetites up to the Curie point. The principal results are:(1) there is no major …

The study of the paleomagnetic signal recorded by rocks allows scientists to understand
Earth's past magnetic field and the formation of the geodynamo. The magnetic recording …

An unpredicted effect of the Verwey transition in magnetite is that a field‐cooled (FC)
remanent magnetization can be less intense than a zero‐field cooled (ZFC) isothermal …

The fundamental temperature dependence of magnetic domain structure has been
recognized for several decades, but its relationship to thermoremanent magnetization (TRM) …

SUMMARY Titanomagnetite containing up to 0.6–0.7 Ti atoms per formula unit is a primary
magnetic mineral phase in submarine basalts and in some terrestrial volcanic rocks. On a …

In addition to classical body domain patterns, a profusion of complex maze like domain
structures have been observed using the Bitter technique on titanomagnetites. Controversy …

Important experiments by Halgedahl (1991) demonstrate that a material can reach
dramatically different domain states on cooling when the experiment is repeated many …