Les séismes de Vrancea sont une série de tremblements de terre dont l'épicentre est massif de Vrancea, dans les « Carpates de courbure » qui se trouve à la jonction de plusieurs micro-plaques tectoniquement actives . La plaque transylvaine avance en direction du sud-est et chevauche les plaques mœsique et scythique à la vitesse d'environ 12 mm par an.
Source: Wikipedia.org
Copyright: Creative Commons 3.0
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