Physics
Scientific paper
May 1999
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999e%26psl.169...59n&link_type=abstract
Earth and Planetary Science Letters, Volume 169, Issue 1-2, p. 59-70.
Physics
3
Scientific paper
Upper Carboniferous through Lower Triassic sediments from Spitsbergen have yielded paleomagnetic results, with those for the Late Gzhelian-Early Permian being the more reliable. The corresponding pole (38°N, 171°E) is fully concordant with the Early Permian segment of the apparent polar wander path for Baltica. It does not support hypotheses about post-Carboniferous mobilism of Spitsbergen with respect to Stable Europe. Neither Mesozoic nor later rifting processes changed the position of Spitsbergen considerably in relation to the Stable Europe.
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