Pesonen L.J.; Elming S.A.; Mertanen S.; Pisarevsky S.; D'Agrella-Filho M.S.; Meert J.G.; Schmidt P.W.; Abrahamsen N.; Bylund G.
(2003)
Palaeomagnetic data are used to study the configurations of continents during the Proterozoic. Applying stringent reliability criteria, the positions of the continents at 12 times in the 2.45- to 1.00-Ga period have been ...