Exhumation kinematics of the Cycladic Blueschists unit and back-arc extension, insight from the Southern Cyclades Sikinos and Folegandros Islands, GreeceReport as inadecuate




Exhumation kinematics of the Cycladic Blueschists unit and back-arc extension, insight from the Southern Cyclades Sikinos and Folegandros Islands, Greece - Download this document for free, or read online. Document in PDF available to download.

1 ISTO - Institut des Sciences de la Terre d-Orléans - UMR7327 2 BRGM - Bureau de Recherches Géologiques et Minières

Abstract : Current models for the Oligo-Miocene post-orogenic back-arc extension of the Aegean domain suggest that stretching is accommodated by two bivergent detachment systems of opposing shear sense. The co-existence in the Eocene of a top-to-the-S thrust at the base of the Cycladic Blueschists unit and top-to-the-N extensional shear zones at the roof raises the problem of differentiating synorogenic and post-orogenic deformations with similar directions and shear senses. Based on structural field data, this study shows that the post-orogenic deformation recorded in the Southern Cyclades is extremely asymmetric as the Cycladic Blueschists unit is pervasively affected by top-to-the-N shearing deformation distributed on four main shear zones. All activated in greenschist-facies conditions, some of these shear zones operated in the brittle regime during the final part of the exhumation. The Cycladic Blueschists-Cycladic Basement contact displays clear polyphased deformation with the preservation of top-to-the-S thrust kinematics. Thermal structure of the Cycladic Blueschists unit with regards to position of ductile shear zones was retrieved using the Raman Spectroscopy of Carbonaceous Material peak-metamorphic temperatures. This study shows a series of major metamorphic gaps accommodating an upward and stepwise decrease of more than 200 °C within the Cycladic Blueschists unit. Pressure-temperature estimates show that only lower parts of the Cycladic Blueschists unit recorded ca. 18–20 kbar for 530 °C peak-conditions. While flanking the West Cycladic Detachment System, which shows a top-to-the-S shear sense, the Southern Cyclades are dominated by a top-to-the-N non-coaxial shearing. Deformation is therefore genuinely asymmetric in the center of the Aegean domain.

Keywords : P-T constraints Back-arc asymmetry. Extensional shear zones Aegean domain Southern Cyclades





Author: Romain Augier - Laurent Jolivet - Leslie Gadenne - Abdeltif Lahfid - Olivier Driussi -

Source: https://hal.archives-ouvertes.fr/



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