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Strongly deformed metaconglomerate layer of the Phyllite-Quartzite unit (Lower high-pressure nappes, External Hellenides). The outcrop surface is parallel to the XZ-principal plane of the strain ellipsoid. The elongated pebbles are mainly quartzites. PhotoID 613

Strongly deformed metaconglomerate layer of the Phyllite-Quartzite unit (Lower high-pressure nappes, External Hellenides). The outcrop surface is parallel to the XZ-principal plane of the strain ellipsoid. The elongated pebbles are mainly quartzites. PhotoID 613

Photograph: Paris Xypolias

Reference: Xypolias, P., Kokkalas, S. 2006. Heterogeneous ductile deformation along a mid-crustal extruding shear zone: an example from the External Hellenides (Greece). In: Law, R.D., Searle, M., Godin, L. (eds) Channel flow, ductile extrusion and exhumation of lower-mid crust in continental collision zones. Geological Society, London, Special Publications, 268, 497-516.