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 …

We describe a modification to existing algorithms for the calculation of first‐order reversal
curve (FORC) diagrams using locally weighted regression smoothing (often referred to as …

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

We present a highly sensitive and accurate method for quantitative detection and
characterization of noninteracting or weakly interacting uniaxial single domain particles …

The aperiodic nature of geomagnetic field variations, both in intensity and direction, can aid
in dating archaeological artefacts, volcanic rocks, and sediment records that carry a …

Magnetic hysteresis measurements of sediments have resulted in widespread reporting of
“pseudo‐single‐domain”‐like magnetic properties. In contrast, the ideal single domain (SD) …

Magnetic hysteresis loops are important in theoretical and applied rock magnetism with
applications to paleointensities, paleoenvironmental analysis, and tectonic studies, among …

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 …

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

Diagenetic alteration of magnetic minerals occurs in all sedimentary environments and
tends to be severe in reducing environments. Magnetic minerals provide useful information …