Paleomagnetic evidence for no tectonic rotation of the Central Italy Tyrrhenian margin since Upper Pliocene

Physics

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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.

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