Dynamics of sedimentary basins and underlying lithosphere at plate boundaries: The Eastern Mediterranean
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Fig. 4

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N-S interpreted seismic section along the STP, Levant Basin and Lattakia Ridge showing the general tectono-stratigraphic architecture of the basin. The STP is separated from the Levant Basin by the Saida fault, marking a sharp contrast between the basin and its southern margin. See Figure 1 for location. Modified from Hawie et al. (2014) and Ghalayini et al. (2014).

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