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Certaines ophiolites--)roches hydratés et minéraux stabilisés dans le domaines du schiste verts---) métamorphismes liés à l'hydrothermalisme accompagnant la lithosphère océanique lors de son expansion-----) préservés pendant la convergence et ps disparue par subduction -------) remontés en surface par un chevauchement de la lithosphère océanique sur une autre lithosphère =OBDUCTIOND'autres ophiolites -) traces de subduction---)roches de minéraux du domaines du schiste bleu ou des éclogites----) entrés en subduction--) métamorphisées à grande profondeur-) exhumés par des contraintes compressives liés à la collision Ophiolites = suture de matériaux océaniques par un affrontement de 2 lithosphères continentales

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