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The small insular group of Mykonos–Delos–Rhenia in Cyclades, Greece, and the southern coast of Turkey from Andriake to Arsuz show three bands of beachrocks, emerged up to +0.35 m and submerged sometimes down to −4.3 m. Because beachrocks are formed within the intertidal zone by carbonate cementation of the beach deposits during stages of shoreline stabilisation (both eustatic and tectonic), they correspond...
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