Ricerc@Sapienza

In the Tyrrhenian back-arc basin, the Ventotene Volcanic Ridge (VR) represents a NW-SEoriented
morphological high, located 25 km north of Ventotene Island in the Eastern Pontine Islands.
It is considered part of an alignment of volcanic edifices developed in the central-eastern Tyrrhenian
Sea, from the western Pontine Islands (WPI) to the Campanian Volcanic Region. The samples dredged
along the VR are basalts to trachybasalts belonging to the transitional (TR) rock-series, with a 40Ar-
39Ar age of 2.760 ± 0.039 Ma. Petrological and geochronological data link the VR basalts to the TR
peralkaline rhyolites cropping out at the WPI (∼1.6-1.1 Ma); here, during a time span of ∼4.5-1.0 Ma
highly differentiated products of high-potassium calc-alkaline (HKCA, ∼4.5-2.9 Ma) and K-alkaline (KA,
∼1 Ma) series were also erupted. Notably, the parental melts of the three rock-series were recognized
in the continental slope close to the WPI (TR, HKCA) and eastward, namely in eastern Pontine Islands
(KA), at the VR (TR), and in the Campanian Plain (HKCA). All the parental melts show typical orogenic
geochemical signatures being originated from a similar heterogeneous suprasubduction mantle source,
without the involvement of anorogenic sources. Tectonically, the faults bordering the VR, associated to the
Pliocene E-W directed rifting stage of the Tyrrhenian back-arc basin were characterized by a more intense
activity during the time span ∼5.0-2.0 Ma (the emplacement time of HKCA and TR series), while KA
products are related to a later stage of extension deformation (<∼2.0 Ma) when the extensional direction
changed to NW-SE and the VR fault activity decreased.