First paleomagnetism of Eocene rocks from Gargano: Widespread overprint or non rotation?

Details First paleomagnetism of Eocene rocks from Gargano: Widespread overprint or non rotation? First paleomagnetism of Eocene rocks from Gargano: Widespread overprint or non rotation?

Dec 1993

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993georl..20.2627s&link_type=abstract

Geophysical Research Letters (ISSN 0094-8276), vol. 20, no. 23, p. 2627-2630

Physics

3

Adriatic Sea, Africa, Europe, Geodynamics, Paleomagnetism, Plates (Tectonics), Rocks, Tectonics, Evolution (Development), Magnetization, Polarity, Rotation

Scientific paper

A paleomagnetic study was carried out in the Gargano Peninsula on 37 sites (500 cores) of mainly Eocene age. Eight normal polarity directions can be interpreted either in terms of remagnetization, or of a small post Middle-Eocene counterclockwise rotation of Adriatic foreland with respect to stable Africa. The reverse directions seem to result from a widespread remagnetization.

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