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A 30-m long piston core from the floor of Pantelleria Trough penetrated an 18 m thick volcaniclastic interval under- and overlain by hemipelagic sediments. The distribution and thickness of the interval is mapped in 3.5 kHz profiles across the trough. Core sediments have been analysed for grain size, carbonate content, detrital petrology, and physical properties such as bulk density and magnetic susceptibility...
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