First‐order reversal curve (FORC) diagrams are rapidly becoming a standard tool for
characterizing magnetic particles because they simultaneously incorporate information …

We have recently developed a technique for characterizing the magnetic components within
natural particle assemblages. This technique is based on the transformation 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 are constructed from a class of partial magnetic
hysteresis loops known as first‐order reversal curves and are used to understand …

From experiments it is known that magnetostatic interactions between grains strongly affect
the magnetic hysteresis behaviour of samples, however, because of the difficulty in …

Theoretical first‐order reversal curves (FORCs) were generated by numerically solving a
thermally activated Stoner‐Wohlfarth model for assemblages of randomly oriented magnetic …

Recently, the study of interacting particles was driven by the modeling effort undertaken to
interpret first‐order reversal curve (FORC) diagrams of natural rocks and sediments …

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 …

First‐order reversal curve (FORC) diagrams are a new technique for identifying magnetic
minerals and characterizing their domain structures and interactions. FORC diagrams have …

Since their introduction in Earth sciences in 1990, first-order reversal curve (FORC)
measurements have become an important tool for characterizing geologic materials. The …