Geomagnetism
Geomagnetism is the study of the dynamics of the Earth’s magnetic field, which is produced in the inner core. The Earth’s magnetic field is predominantly a geo-axial dipole, with north and south magnetic poles located near the geographic poles that undergo periodic reversals and excursions.
Featured
Latest Research and Reviews
-
Research
| Open AccessEarly Cambrian renewal of the geodynamo and the origin of inner core structure
Nature Communications 13, 4161 -
-
Research
| Open AccessThe accuracy of geostatistics for regional geomagnetic modeling in an archipelago setting
Scientific Reports 12, 7441 -
-
Research
| Open AccessNew magnetic anomaly map for the Red Sea reveals transtensional structures associated with rotational rifting
Scientific Reports 12, 5757 -
Research
| Open AccessIntermittent non-axial dipolar-field dominance of twin Laschamp excursions