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Deformation within the Cycladic subduction–exhumation channel: new insights from the enigmatic Makrotantalo nappe (Andros, Aegean)

  • N. Gerogiannis
  • P. XypoliasEmail author
  • V. Chatzaras
  • E. Aravadinou
  • K. Papapavlou
Original Paper

Abstract

New detailed geological/structural mapping coupled with microstructural investigations and amphibole chemistry analyses are used to elucidate the enigmatic tectonic evolution of the Makrotantalo nappe on northern Andros (Aegean region). On the basis of the new geological map, we re-evaluate the structural position of samples with previously published metamorphic ages to show that the Makrotantalo nappe has been affected by the early Eocene high-pressure (HP) metamorphism. Therefore, the Makrotantalo nappe is an integral part of the Cycladic Blueschist Unit (CBU). The early, main ductile deformation phase recognized in the mapped area, is associated with the emplacement of the Makrotantalo nappe over the North Cyclades nappe at deep subduction levels during early Eocene. The subsequent deformation phase occurred at the middle Eocene–Oligocene synchronous with the decompression of blueschist rocks from the stability field of glaucophane to that of actinolite. During this phase, the nappe pile was folded by map-scale folds, which were locally transposed by ductile shear zones. These shear zones were related with NE-directed oblique thrusting and, locally, either restacked the nappe pile or reworked the early nappe contact. Our results in combination with previous studies in the northern Cyclades show that the top-to-the-NE shearing was dominant at a large part of the CBU during exhumation. Opposite, SW-directed shearing was restricted at the upper structural levels of the CBU. We suggest that the observed spatial variation in shear sense is compatible with NE- rather than SW-directed ductile extrusion of the CBU.

Keywords

Blueschists Ductile deformation Quartz fabrics Amphibole chemistry Ductile extrusion Hellenides 

Notes

Acknowledgements

We are grateful to Michael Bröcker, Giancarlo Molli and Uwe Ring for their constructive review comments as well as to Wolf-Christian Dullo for editorial handling. Thanks are also due to I. Koukouvelas and S. Kokkalas for insightful discussions in the field. We acknowledge the contribution of the ex-students C. Karavoulia, G. Gkekas, P. Kapizionis, D. Sereti, D. Vlassi, A. Kapoutsi and K. Theofani from the University of Patras who mapped parts of the study area in the course of their Bachelor thesis. The staff of the Laboratory of Electron Microscopy & Microanalysis (Univ. Patras) is also acknowledged for their support. Fieldwork for this study was supported by Grant C.924 (awarded to P. Xypolias) from the Research Committee of the University of Patras (Programme K. Karatheodori).

Supplementary material

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Copyright information

© Geologische Vereinigung e.V. (GV) 2019

Authors and Affiliations

  1. 1.Department of GeologyUniversity of PatrasPatrasGreece
  2. 2.School of GeosciencesThe University of SydneySydneyAustralia
  3. 3.GEOTOPUniversité du Québec à MontréalMontrealCanada

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