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The Changing Roles of Long-lived Faults in MountainBelts: Examples from the Variscides of Southern Ireland

Once initiated and developed, faults tend to have prolongedactivation histories that highly influence tectonic deformation, fluid flow, andassociated mineralisation in the brittle upper crust. The fault systems associated with Devonian/Carboniferous crustal extension and subsequent Variscan crustal shortening from southern Ireland … Continue reading