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More model informationThis submarine channel exposure is from the Miocene age Gorgoglione Flysch Formation and outcrops above the town of Castelmezzano Italy (PZ). This outcrop features a primary channel surface incising into underlying tabular-bedded frontal lobe deposits. Above the primary channel surface are very coarse-grained conglomerates and amalgamated coarse sandstone channel fill deposits.
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Oct 18th 2014
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