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

Archaeomagnetic data are fundamental for our understanding of the evolution of Earth's
magnetic field on centennial to millennial timescales. From the earliest studies of the …

The strength of the geomagnetic field has decreased rapidly over the past two centuries,
coinciding with an increasing field asymmetry due to the growth of the South Atlantic …

Background GEOMAGIA50. v3 is a comprehensive online database providing access to
published paleomagnetic, rock magnetic, and chronological data from a variety of materials …

Study of the late Quaternary geomagnetic field contributes significantly to understanding the
origin of millennial‐scale paleomagnetic secular variations, the structure of geomagnetic …

We propose a global geomagnetic field model for the last 14 thousand years, based on
thermoremanent records. We call the model ArchKalmag14k. ArchKalmag14k is constructed …

Geomagnetic dipole moment variations associated with polarity reversals and excursions
are expressed by large changes of the cosmogenic nuclide beryllium‐10 (10Be) production …

Reconstructions of the geomagnetic field on long time scales are important to understand
the geodynamo processes in the Earth's core. The geomagnetic field exhibits a range of …

Long-term variations of the geomagnetic dipole moment (GDM) during periods of stable
polarity and in transitional states (reversals and excursions) provide key information for …

The geomagnetic field prevents energetic particles, such as galactic cosmic rays, from
directly interacting with the Earth's atmosphere. The geomagnetic field is not static but …