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Pyroclastic deposits at the base of dacitic dome (grey in color). Photo ID 640

Pyroclastic deposits at the base of dacitic dome (grey in color). Photo ID 640

Photograph: Alessandro Da Mommio

Reference: The transition from subduction arc to slab tearing: Evidence from Capraia Island, northern Tyrrhenian Sea. Massimo Gasparona, Gideon Rosenbauma, Jan Wijbransb, Piero Manetti