Data for: Continuous millennial decrease of the Earth’s magnetic axial dipole
Published: 8 June 2018| Version 1 | DOI: 10.17632/bdt5csrxc9.1
Contributors:
Wilbor Poletti, , , , Description
Archaeointensity dataset for the last two millennia, selected from the reassessment of the GEOMAGIA50 database (Brown et al., 2015) and recent estimates that had not yet therein. These data were used in the calculation archaeo_adm_1.3k model, which suggested a continuous decrease of the Earth’s magnetic axial dipole from ~ 750 CE to present.
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Categories
Geomagnetism, Paleomagnetism