An Upper Cretaceous paleomagnetic pole for stable Europe from Aix-en-Provence (France)

Details An Upper Cretaceous paleomagnetic pole for stable Europe from Aix-en-Provence (France) An Upper Cretaceous paleomagnetic pole for stable Europe from Aix-en-Provence (France)

Aug 1989

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1989e%26psl..94..143w&link_type=abstract

Earth and Planetary Science Letters, Volume 94, Issue 1-2, p. 143-150.

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Scientific paper

A paleomagnetic study of continental deposits (limestones, sandstones) from the Upper Cretaceous basin of Aix-en-Provence (Campanian to Danian) (43.5°N, 5.5°E) gives a mean paleomagnetic direction of: D = 9.5°, I = 46.8°, N = 10, k = 33, α95 = 8.3° and a mean pole: 73°N, 156°E, N = 10, K = 24, A95 = 10°. The fold test is positive, as is the reversal test. This pole is not significantly different from other Cretaceous or lower Tertiary poles from stable Europe.

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