Dynamics of sedimentary basins and underlying lithosphere at plate boundaries: The Eastern Mediterranean
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[1] (A) Studied outcrop near Koilani village (34°50′15.52N; 32°51′31.12E); (B) Thin bedded bioclastic grainstones; (C) Photomicrographs (PPL – Plane Polarized) of packstone/grainstones with abundant benthic and pelagic foraminifera; (D) Traces of mega-ripples in a bioclastic grainstone; [2] (A) Studied outcrop of the upper Pakhna Formation in the eastern part of Limassol Basin (34°43′19.76N; 33°1′2.19E); (B) Grainstones interbedded with wackestones; the base of the calcarenitic unit is composed of allochthonous grains; (C) Bioturbated w/p grading to grainstone; (D) Photomicrograph (PPL – Plane Polarized) of calcarenite with shell debris and quartz.

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