Exploring geomagnetic field behaviour during polarity reversals and excursions
The Earth's magnetic field, which is driven by dynamo action within the molten outer core, is constantly changing. Variations occur over a wide range of both spatial and temporal scales, and contribute to a complex overall field morphology. Despite significant advances over the last 25 years, much remains unknown regarding the behaviour and driving mechanisms of the geomagnetic field, with increased understanding requiring collection of further high-quality paleomagnetic records and development...[Show more]
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