Paleomagnetic records from sediments, archeological artifacts, and lava flows provide the
foundation for studying geomagnetic field changes over 0–100 ka. Late Quaternary time …

After many years spent by paleomagnetists studying the directional behavior of the Earth's
magnetic field at all possible timescales, detailed measurements of field intensity are now …

We present a new model of the magnetic field at the core–mantle boundary for the interval
1590–1990. The model, called gufm1, is based on a massive new compilation of historical …

We have constructed new apparent polar wander paths (APWPs) for major plates over the
last 200 Myr. Updated kinematic models and selected paleomagnetic data allowed us to …

A Simplified Statistical Model for the Geomagnetic Field and the Detection of Shallow Bias
in Paleomagnetic Inclinations: Was th Page 1 A Simplified Statistical Model for the …

We present a synthesis of 0–5 Ma paleomagnetic directional data collected from 17 different
locations under the collaborative Time Averaged geomagnetic Field Initiative (TAFI). When …

Because of paleomagnetic inclination error (I error) in sedimentary rocks, we argue that
previous estimates of Triassic and Jurassic paleolatitudes of the North American craton have …

Magnetostratigraphy of 222 remanent directions together with late Oligocene to early
Miocene mammal and charophyte paleontology suggest that 2179 m of the **shuigou …

The magnetic field of the Earth is by far the best documented magnetic field of all known
planets. Considerable progress has been made in our understanding of its characteristics …

The dipole moment of Earth's magnetic field has decreased by nearly 9\% over the past 150
years and by about 30% over the past 2,000 years according to archeomagnetic …