The basins and orogens of the Mediterranean region ultimately result from the opening of
oceans during the early break-up of Pangea since the Triassic, and their subsequent …

The selection of paleointensity data is a challenging, but essential step for establishing data
reliability. There is, however, no consensus as to how best to quantify paleointensity data …

Palaeomagnetic field intensity measurements, derived from rocks with ages that span
geological time, provide a crucial constraint on the evolution of Earth's deep interior and its …

Globally distributed paleomagnetic data from discrete volcanic sites have previously been
used for statistical studies of paleosecular variation and the structure of the time‐averaged …

Apparent polar wander paths (APWPs) calculated from paleomagnetic data describe the
motion of tectonic plates relative to the Earth's rotation axis through geological time …

Records of reversal frequency support forcing of the geodynamo over geological timescales
but obtaining these for earlier times (eg, the Precambrian) is a major challenge. Changes in …

Investigations into long‐term geomagnetic variations provide useful information regarding
paleomagnetic field behavior. In this study, we assess the latitudinal structure of …

Nonideal, nonsingle-domain magnetic grains are ubiquitous in rocks; however, they can
have a detrimental impact on the fidelity of paleomagnetic records—in particular the …

The minerals carrying the magnetic remanence in geological samples are commonly a solid
solution series of iron‐titanium spinels known as titanomagnetites. Despite the range of …

Secular variation, the change in the Earth's magnetic field through time, reflects the energy
state of the geodynamo. Secular variation is commonly quantified by paleomagnetists as the …