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The structure, age and facies distribution of the sedimentary substrate of the Colli Albani volcano has been investigated by analysing sedimentary xenoliths enclosed in pyroclastic and phreatomagmatic deposits from different eruptive centres of the volcano, for comparison with the stratigraphies of deep wells drilled in the area and the known surface geology of the areas surrounding the volcano. Thin-section analysis has been carried out on the same xenolith samples collected and discussed by Funiciello and Parotto (1978. Il substrato sedimentario nell’area dei Colli Albani: considerazioni geodinamiche e paleogeografiche sul margine tirrenico dell’Appennino Centrale. Geologica Romana, 17,...

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