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Mudcracks in the Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Mudcracks were formed on the surface of sedimentation lagoons during dry periods in a tropical climate. Gorges du Cians, Dome du Barrot

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