Figure 14.

Schematic 3D block diagram and related cross‐section model for the tectonic evolution of the Evia Shear Zone from subduction thrusting of the Basal Unit (a), syn‐orogenic extrusion (b), and post‐orogenic unroofing and coaxial flattening (c). Basal Unit flysch within the Evia Shear Zone records syn‐convergence fabrics and structures that were partially, or locally totally, overprinted during exhumation by structures related to flattening and consequent vertical ductile thinning. See text for details.