Skip to Main Content
Skip Nav Destination

Major- and trace-element and Sr-Nd-Pb isotope compositions are presented for an extensive data set of samples (44) recovered along the active ridge axis of the southern Tyrrhenian backarc basin represented by the Marsili volcano (<0.7 Ma). In addition, major and trace elements are presented for the few lavas sampled from the summit area (active at 0.4–0.1 Ma) of Vavilov volcano, located in the oceanic subbasin (i.e., Vavilov Basin) formed during the first stage of the southern Tyrrhenian backarc basin formation.

Overall, these data confirm that southern Tyrrhenian backarc basin magmatism is chemically heterogeneous, ranging from an island-arc basalt (IAB) type,...

You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
Close Modal

or Create an Account

Close Modal
Close Modal