Coimbra (Sé Nova), Portugal
Vigo, España
Zaragoza, España
The palynological and palaeomagnetic data obtained from the Vale da Mó and Monçarros Formations are presented. The Palaeomagnetic results from the upper beds of the Monçarros Formation allowed the definition of a magnetic component (dec./inc. = 156.5°/14.4°; K=206.4, ct95=8.6°) acquired during stephano-permian times sedimentation in a mostly reversed field at low southern latitude.
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