Dynamics of sedimentary basins and underlying lithosphere at plate boundaries: The Eastern Mediterranean
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Fig. 3

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Stratigraphic logs and correlation between Terbol-1 (north) and Adloun-1 (south) coastal wells showing the thickness variation of the variation of Cretaceous sequences between the northern and southern margins of Lebanon. These wells are the most proximal to the eastern margin of the Levant Basin (for locations check Figs. 1 and 9). Modified from Ukla (1970) and Beydoun (1977).

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