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Following the Last Glacial Maximum (LGM) lowstand, global sea-level rose by ~120m flooding previously exposed continental shelves worldwide with water and sediments. In these drowned environments sediment accumulation patterns are dictated by a superposition of vertical tectonic motion, sea-level change and sediment supply rates, which are hard to distinguish from one another. This study focuses on...
Paleodepth reconstructions of the late Tertiary Levant continental margin off Israel, using one- and two-dimensional quantitative basin analysis, reveals several interesting phenomena in the evolution of the margin, such as: tilting events of the deep basin in north–south and east–west directions; westward progradation of the continental shelf in the southern Levant; and the variation in style along...
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