Retrogression of eclogite-facies shear zones by short-lived fluid infiltration during the Caledonian orogeny, Lofoten islands, Norway

• Main Authors: H. W. Fournier, J. K. W. Lee, A. Camacho, R. A. Creaser
• Format: Dataset
• Language: unknown
• Published: Geological Society of London 2016
• Subjects: Geology; FOS Earth and related environmental sciences; Lofoten; Norway
• Online Access: https://dx.doi.org/10.6084/m9.figshare.3453545.v1; https://geolsoc.figshare.com/articles/dataset/Retrogression_of_eclogite-facies_shear_zones_by_short-lived_fluid_infiltration_during_the_Caledonian_orogeny_Lofoten_islands___Norway/3453545/1

Norwegian eclogite-facies shear zones in the Lofoten islands served as major pathways for short-lived pulses of both 40 Ar-rich and 40 Ar-poor hot fluids during eclogitization and retrogression events related to the Caledonian orogeny. The open system for Ar affected most of the minerals leading to old 40 Ar/ 39 Ar ages, particularly in trioctahedral micas. 40 Ar concentration in the fluids appears to decrease during the amphibolite-facies retrogression and Ca-rich amphiboles yield 40 Ar/ 39 Ar ages of c. 415 Ma (Scandian event). Late- and post-Caledonian 40 Ar/ 39 Ar muscovite and K-feldspar ages and Rb/Sr biotite ages coincide with multiple extensional events, fluid infiltration and thermal activity during the final exhumation of the crustal rocks, potentially reflecting major tectonic episodes such as rifting of Pangaea and seafloor spreading between Europe and North America.