First‐order reversal curve (FORC) diagrams of synthetic binary mixtures with single‐domain,
vortex state, and multidomain end‐members (EMs) were analyzed using principal …

We describe a quantitative magnetic unmixing method based on principal component
analysis (PCA) of first‐order reversal curve (FORC) diagrams. For PCA, we resample FORC …

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

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 …

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 have recently been used for the characterization
of magnetic systems in both geology and physics. However, the FORC distribution involves …

We describe a method for simulating first‐order reversal curve (FORC) diagrams of
interacting single‐domain particles. Magnetostatic interactions are calculated in real space …

First-order reversal curve (FORC) diagrams were modelled and experimentally measured
for different assemblages of single-domain (SD) magnetite particles with bimodal …

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

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