Many of the natural materials studied in rock and environmental magnetism contain a mixed
assemblage of mineral grains with a variety of different origins. Mathematical decomposition …

Single‐domain magnetite particles produced by magnetotactic bacteria (MTB) and aligned
in chains, called magnetosomes, are potentially important recorders of paleomagnetic …

Natural sediments are a complex mixture of magnetic minerals with different origins and
different geochemical history, each of which is called a magnetic component. Magnetic …

Susceptibility, thermo-remanent magnetization (TRM) and isothermal remanent
magnetization (IRM) anisotropy ellipsoids have been determined for several rock samples …

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

The acquisition of isothermal remanent magnetization (IRM) curves through the application
of stepwise-increasing uniaxial fields to a rock-magnetic sample provides an important non …

The first theoretical predictions for the behavior of magnetic particles in water were that
sedimentary magnetizations would be fully aligned with the ambient field, yet redeposition …