Variations of the Earth's Magnetic Field

Study paleointensity recorded in rocks and archaeological artifacts and their variations in different time scales, with implications in defining the age of formation of the Internal Core (solid), the conductivity of the mantle and the influences of variations in the intensity of the geomagnetic field on the climate.

Related articles:

Archeointensity in Northeast Brazil over the past five centuries

Time evolution of the South Atlantic Magnetic Anomaly