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

In many geomagnetic, geological and environmental magnetic studies, it is important to
have reliable methods of characterizing the composition and grain size distribution of …

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 …

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 …

Paleomagnetic and environmental magnetic studies are commonly conducted on samples
containing mixtures of magnetic minerals and/or grain sizes. Major hysteresis loops are …

First‐order reversal curve (FORC) diagrams were measured on a variety of synthetic and
natural (submarine basalts and potsherds) samples, as well as for a mixture, between room …

First‐order reversal curve (FORC) diagrams for mixtures of different magnetic phases and
bimodal distributions have been measured to examine the efficiency of the FORC method at …

Domain state and mixing analysis based on isothermal magnetization measurements is
often restricted to the use of the Day plot. In order to make more information from simple rock …

The recently developed first-order reversal curve (FORC) technique for rapidly examining
magnetic domain state has great potential for paleomagnetic and environmental magnetic …

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