Detailed palaeomagnetic sampling has been made of two units of the Middle Triassic in the western Cordillera Ibérica in Central Spain. Thermal demagnetization reveals the preservation of characteristic Triassic remanence. A recent overprint is also present, but it is almost completely removed after 5000 C. A magnetostratigraphic section was constructed based upon the isolated stab/e components related to the higher unblocking temperature
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