Dynamics of sedimentary basins and underlying lithosphere at plate boundaries: The Eastern Mediterranean
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Fig. 7


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[1] (A) Photograph showing a turbidite system in the Limassol Basin (34°48′23.30N; 32°47′29.49E); (B) Wackestone grading to packstone; (C) Highly bioturbated mudstone grading to packstone; [2] (A) Micritic non-porous mudstone, rich in pelagic foraminifera; (B) Cross-bedded grainstones fining to marlstones; (C) Mudstone overlain by gross bedded grainstones suggesting the initiation of a new cycle; [3] (A) Panoramic view of the MTCs identified along the Limassol-Pafos highway (34°45′21.30N; 34°45′21.30E); [4] (A) Studied outcrop of basinal sediments near Monagri village (34°47″16.07″N; 32°54′53.99″E); (B) Alternations of mudstone/wackestones with packstones; (C) Highly bioturbated mudstone; (D) Photomicrograph (PPL – Plane Polarized) of wackestone with benthic and planktonic foraminifera.

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