Integration of palaeomagnetic data and numerical dynamo simulations support a moderately dipolar geomagnetic field throughout Earth history
Andrew John Biggin1, Richard Bono2, Courtney Jean Sprain3, Christopher J Davies4, Richard T Holme5, Pavel V Doubrovine6 and Domenico Meduri2, (1)University of Liverpool, Department of Earth, Ocean and Ecological Sciences, Liverpool, L69, United Kingdom, (2)University of Liverpool, Liverpool, United Kingdom, (3)University of Florida, Department of Geological Sciences, Gainesville, FL, United States, (4)University of Leeds, School of Earth and Environment,, Leeds, United Kingdom, (5)Univ Liverpool, Liverpool, United Kingdom, (6)University of Oslo, Oslo, Norway
