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. Dans-le-cas-du-sud-de-i-'espagne, des études basées sur I'interprétation des paragenèses ont permis d'approcher I'historique de métamorphisme du complexe Nevado-Fillabride (Figure9) Cependant, aucune étude ne lie I'historique géologique aux microstructures de calcite rencontrées dans les marbres du domaine. D'après les études citées ci-dessus, un lien entre l'historique géologique et la microstructure des marbres de Macael peut être établi, Nous exposons dans ce qui suit quelques données et réferences utiles au développement de ce lien