Quaternary alluvial deposits of Wadi Gaza in the middle of the Gaza Strip (Palestine): Facies, granulometric characteristics, and their paleoflow direction
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Identify the lithofacies of the Wadi Gaza, focusing on the coarse-grained deposits.

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Sphericity values of the coarse grains increase toward the west direction.

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Source of sediments is Beir Sheva, the Northern Negev, and Hebron mountains.

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Two periods of climate conditions were depicted.

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