New insights on the Late Quaternary geologic evolution of the Ischia Island coastal belt based on high-resolution seismic profiles

The study of the seismo-stratigraphic architecture of Late Quaternary-Holocene volcanic andsedimentary units in the Ischia Island offshore and their correlation with the coastal units of theadjacent onshore sectors allowed for a detailed reconstruction of the seismic stratigraphy of thenorthern, southern and western sectors of the island. Five (southern Ischia) to nine (western Ischia)seismic units and related seismic facies were identified. The volcanic areas and their detailedseismo-stratigraphic setting fit well in the geological context of a passive margin and confirm thatthe stratal architecture in the Ischia Island Quaternary marine deposits is controlled by theinteraction between glacio-eustatic fluctuations, volcanism, tectonics and sedimentary supply.