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L'analyse structurale de failles extensives des monts du Mâconnais démontre l'existence de phénomènes extensifs de faible intensité, situés en arrière de la marge passive de la Téthys ligure, dont l'axe était, au Jurassique moyen, situé à environ 400 km au sud-est du secteur étudié. Les mesures des directions de courants de retour de tempêtes et l'examen de la position de lentilles de coraux suggèrent...
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