Survol des limites d’âge de la minéralisation aurifère dans le centre et l’ouest de Terre-Neuve et des nouvelles datations 40Ar/39Ar de la muscovite de certaines zones aurifères
DOI :
https://doi.org/10.4138/atlgeo.2022.012Résumé
La présente contribution fait état de nouvelles données obtenues par chauffage échelonné au laser 40Ar/39Ar de muscovite associée à quatre zones minéralisées aurifères orogéniques stratégiques dans le centre et l’ouest de Terre-Neuve permettant de mieux préciser les limites géochronologiques existantes de la minéralisation aurifère orogénique dans la majeure partie des Appalaches terre-neuviennes. Nous fournissons de plus les premières données par chauffage échelonné au laser 40Ar/39Ar de muscovite détritique provenant de grès minéralisé aurifère de la Formation de Wigwam (groupe de Botwood) dans la zone d’intérêt aurifère de Moosehead. La majorité des zones aurifères connues sur l’île se trouve à proximité de failles d’échelle crustale et de structures connexes, et elles se situent communément à l’intérieur d’unités lithologiques rigides parallèles (p. ex. des roches granitiques), bien que certains réseaux filoniens recoupent des séquences de roches sédimentaires clastiques moins parallèles. L’âge des roches hôtes varie du Néoprotérozoïque au Dévonien et peut s’étendre au Carbonifère. Des datations robustes du Praguien à l’Emsien (env. 410 à 375 Ma) de rutile, de muscovite et de zircon limitent le moment de la minéralisation de l’or dans des parties de la sous-zone Exploits, alors que des estimations moins précises de l’âge de la minéralisation aurifère dans la sous-zone Notre-Dame et de la marge laurentienne varient du Wenlock à l’Emsien (env. 433 à 375 Ma). Les données géochronologiques laissent collectivement supposer que les cycles de pression hydraulique associés à la minéralisation d’or dans le centre et l’ouest de Terre-Neuve se sont manifestés durant la progression tectonique siluro-dévonienne associée aux stades de ralentissement du cycle orogénique salinique et s’étendant aux cycles orogéniques acadien et néoacadien. Plusieurs phénomènes orogéniques polyphasés se chevauchant ont permis des écoulements de fluides minéralisateurs aurifères répétés, en particulier à proximité de zones de failles d’échelle crustale réactivées persistantes.
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