A wide variety of Earth and planetary materials are very good recorders of paleomagnetic
information. However, most magnetic grains in these materials are not in the stable single …

The term “pseudo‐single domain”(PSD) has been used to describe the transitional state in
rock magnetism that spans the particle size range between the single domain (SD) and …

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 …

First-order reversal curve (FORC) diagrams have been experimentally shown to be a better
way of discriminating domain states in a sample compared to the straightforward use of …

The thermal demagnetization of pseudo‐single‐domain (PSD) magnetite (Fe3O4) particles,
which govern the magnetic signal in many igneous rocks, is examined using off‐axis …

The magnetic domain state of a material determines its magnetic recording capability and
magnetic properties. Constraining the domain state of magnetic components within …

Reliability of magnetic recordings of the ancient magnetic field is strongly dependent on the
magnetic mineralogy of natural samples. Theoretical estimates of long‐term stability of …

Dusty olivine (olivine containing multiple sub-micrometer inclusions of metallic iron) in
chondritic meteorites is considered an ideal carrier of paleomagnetic remanence, capable of …

The thermomagnetic behavior of remanence‐induced magnetite (Fe3O4) particles in the
pseudo‐single‐domain (PSD) size range (~ 0.1–10 µm), which dominate the magnetic …

First-order reversal curve (FORC) diagrams are used increasingly in geophysics for
magnetic domain state identification. The domain state of a magnetic particle is highly …