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 …

We tested single‐domain (SD) and multidomain (MD) theories of the acquisition and thermal
demagnetization of thermoremanent magnetization (TRM) and partial TRM (pTRM) in …

Hematite carries magnetic signals of interest in tectonic, paleoclimatic, paleomagnetic, and
planetary studies. First‐order reversal curve (FORC) diagrams have become an important …

Rock magnetic studies of complex systems that contain mixtures of magnetic minerals or
mixed grain size distributions have demonstrated the need for a better method of …

Besides granites of the ilmenite series, in which the anisotropy of magnetic susceptibility
(AMS) is mainly controlled by paramagnetic minerals, the AMS of igneous rocks is …

The multispecimen protocol (MSP) is a method to estimate the Earth's magnetic field's past
strength from volcanic rocks or archeological materials. By reducing the amount of heating …

The central ridge structure of a first‐order reversal curve (FORC) distribution is indicative of
uniaxial noninteracting single domain magnetic particles, which provides the opportunity to …

It is widely accepted that cooling rate can strongly influence the intensity of the thermal
remanent magnetization (TRM) acquired by rocks during cooling to ambient temperatures. If …

Obtaining reliable estimates of the absolute palaeointensity of the Earth's magnetic field is
notoriously difficult. The heating of samples in most methods induces magnetic alteration—a …

The Thellier technique is the most commonly used method for absolute palaeointensity
studies. It is based on Thellier's laws stating that partial thermoremanent magnetisations …