First‐order reversal curve (FORC) diagrams are constructed from a class of partial magnetic
hysteresis loops known as first‐order reversal curves and are used to understand …

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

Abstract The “Day” diagram (Day et al., 1977, https://doi. org/10.1016/0031-9201 (77) 90108-
X) is used widely to make inferences about the domain state of magnetic mineral …

High-resolution first-order reversal curve (FORC) diagrams are increasingly employed to
characterize magnetic minerals in sediments, and especially as a magnetofossil detection …

Iron oxide nanoparticles are of interest in a wide range of biomedical applications due to
their response to applied magnetic fields and their unique magnetic properties …

First‐order reversal curve (FORC) diagrams have become a standard tool in rock
magnetism, yet magnetite is the only magnetic mineral that is well characterized using …

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 …

Magnetic techniques are suitable to detect iron oxides even in trace concentrations.
However, since several iron oxides may be simultaneously present in natural and synthetic …

We present results for a series of hysteresis measurements that provide information about
remanent, induced, transient‐free, and transient magnetization components. These …

The Nihewan fluvio-lacustrine sequence (North China) has recorded late Pliocene–
Pleistocene climatic and environmental changes, and contains valuable information on early …