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- W1918673652 abstract "Reliques antithetiques de la phase primitive du cisaillement Nord Armoricaine (Bretagne, France). La zone de cisaillement nord armoricaine (NASZ) (Bretagne, France) orientee E-W et active au Paleozoique est reconnue comme une zone de cisaillement dextre intracontinentale. La zone cataclasique de Queffleuth (QCZ) a ete definie dans la vallee de Queffleuth au sein de la NASZ. La QCZ contient des protocataclasites a des cataclasites. Dans la QCZ, quatre classes morphologiques de failles ont pu etre petrographiquement definies. Perpendiculairement au plan de failles de la premiere classe, le pourcentage de matrice augmente tandis que le pourcentage de clastes diminue, en s'eloignant du plan de faille. De ce fait, cette classe est interpretee comme pene-contemporaine des cataclasites. Les trois autres classes recoupent les cataclasites et sont ainsi datees post-cataclase. Il a ete remarque que l’orientation privilegiee des failles etait N-S. Une analyse en termes de tenseurs de contrainte a permis d’identifier cinq evenements coherents. La predominance de la direction N-S a ete interpretee comme une expression antithetique par rapport au mouvement general de la NASZ. Il en resulte la recurrente de mouvements dextres et senestres de la QCZ pendant et apres la phase de cataclase. Ainsi on propose une alternance de plusieurs tenseurs de contraintes pendant la phase primitive du cisaillement nord armoricain, comme dans la zone sismique du sud de l’Islande." @default.
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- W1918673652 date "2013-04-23" @default.
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- W1918673652 title "Antithetic-dominated relics of the immature stage of the North-Armorican shear zone (Brittany, France)" @default.
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