Palaeomagnetism of a slowly cooled plutonic terrain in western Greenland

Details Palaeomagnetism of a slowly cooled plutonic terrain in western Greenland Palaeomagnetism of a slowly cooled plutonic terrain in western Greenland

Feb 1976

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1976natur.259..382m&link_type=abstract

Nature, Volume 259, Issue 5542, pp. 382-385 (1976).

Physics

14

Scientific paper

PALAEOMAGNETIC results from a high grade Precambrian terrain in western Greenland show many features attributable to magnetisation during very slow cooling caused by gradual uplift and erosion. They may locate a whole segment of the Laurentian apparent polar wander (APW) path with unusually high precision and also indicate the probable direction of movement.

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