X. Barberà, Lluís Cabrera Pérez, E. Gomis Coll, Josep Maria Parés Casanova
A paleomagnetic study was carried out in Oligocene-Miocene fluvial and lacustrine sediments of the Ebro Basin. A significative number of samples are treated. A Paleomagnetic Pole for the OligoceneMiocene boundary in the Ebro Basin has been obtained (Lat. = 79.6° N, Long. = 155.9° E, lX 9S= 5.9). This results indicate no significative rotations for the Ebro Basin since the upper Oligocene.
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