Physics
Scientific paper
Mar 1994
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1994georl..21..481s&link_type=abstract
Geophysical Research Letters (ISSN 0094-8276), vol. 21, no. 6, p. 481-484
Physics
9
Demagnetization, Earth Crust, Geomagnetism, Italy, Paleomagnetism, Rotation, Tectonics, Clays, Geodynamics, Stratigraphy
Scientific paper
We present paleomagnetic results from 141 samples collected at 12 sites from Plio-Pleistocene clayey units in the extensional Central Italy Tyrrhenian margin. All samples were subjected to stepwise alternating field and/or thermal demagnetization. Positive fold and reversal tests indicate that the results refer to a primary component of magnetization. Paleomagnetic mean direction (Declination = 358.0 deg; Inclination = 55.2 deg; alpha(sub 95) = 4.1 deg) reflects the expected geocentric axial dipole field for the locality, thus indicating that this sector of the Tyrrhenian margin did not undergo any tectonic rotation during the past 4 million years.
Faccenna Claudio
Funiciello Renato
Mattei Massimo
Sagnotti Leonardo
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