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The 39 ka campanian ignimbrite eruption: New data on source area in the campanian plain
2019The Piperno eutaxitic tuff, 20 m thick, interfingered with loose lithic-rich breccia, that outcrops at the base of Camaldoli hill (Campi Flegrei) (De Lorenzo, 1904) was interpreted by Rittmann (1950) to be a local air fall tuff. This welded tuff was reinterpreted by Rosi et al.
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