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he dominant feature in the magnetic declination record at all European sites for which adequate data are available is a minimum between 1750 and 1860. The time of minimum at different sites correlates...
Palaeomagnetic Evidence for the Drift of the Fennoscandian Field
palaeomagnetism Fennoscandia Precambrian continental drift palaeolatitude
2009/6/10
The basic requirements of reliable palaeomagnetic data for calculation of continental drift and past plate reconstructions are that the Natural Remanent Magnetization is primary, separated from younge...
On the Shape of the Fast Ice - Drift Ice Contact Zone
fast ice boundary fracture mechanics Baltic Sea
2009/6/9
The location and the geometry of the fast ice zone are examined in the Bay of Bothnia, Baltic Sea.Remote sensing images were collected from the fast ice – drift ice boundary zone showing that the fast...