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Publications by [Sartori R.]

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A deep, narrow, and distorted Benioff zone, plunging from the Ionian Sea towards the southern Tyrrhenian basin, is the remnant of a long and eastward migrating subduction of eastern Mediterranean lithosphere. From Oligocene to Recent, subduction generated ...
Filed under: Geology -  General Geology
Reference: 32nd International Geological Congress, Episodes Vol.26 No.3