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We conducted a paleomagnetic study on late Ediacaran and early Cambrian volcanic deposits and lava flows from the Ouarzazate and Taroudannt groups in the Anti-Atlas, Morocco. Four stable magnetic mean directions have been isolated using thermal demagnetization technique. A first component “A” is most probably a remagnetization acquired during the Hercynian related tectonic phases, and yields a paleomagnetic...
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