Palaeomagnetic observations are being used in increasingly sophisticated geological and
geophysical interpretations. It is therefore important to test the theories behind …

Magnetic measurements of samples with precisely controlled magnetic mineralogy, grain
size, and interparticle spacing are needed to provide crucial experimental rock magnetic …

A suite of near‐identical magnetite nanodot samples produced by electron‐beam
lithography have been used to test the thermomagnetic recording fidelity of particles in the …

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 …

Insight into the size and morphology of assemblages of magnetite particles can be gained
by comparing temperature variations of remanence or susceptibility after zero‐field cooling …

We have measured initial susceptibility χ0 and the dependence of anhysteretic rémanent
magnetization (ARM) and thermoremanent magnetization (TRM) on applied field for seven …

Experiments designed to measure the absolute palaeointensity of the geomagnetic field
generally do so by comparing the ancient thermoremanent magnetization (TRM) retained by …

Despite the influence that paleomagnetism has exerted on the earth sciences, our
understanding of thermal remanent magnetization (TRM), which is one of the primary …

It has long been hypothesized that the pseudo‐single‐domain properties of submicron
magnetites are a result of coexisting multidomain and single‐domain‐like remanences. We …

Magnetic measurements at cryogenic temperatures (< 300 K) proved to be useful in
paleomagnetic and rock magnetic research, stimulating continuous interest to low …