Geochemical and petrological investigations of the volcanic islands of
Christiana proved their genetic connection with the calc-alkaline volcanism of the
Santorini group and the submarine Kolombos volcano. The lavas of Christiana
range from andesite to dacite while pumice is of rhyolithic chemistry. Rather
constant K/Rb ratios indicate consanguine magmas.
Increased Ni, Cr and Mg concentrations in several lavas indicate a certain
admixture of peridotite material to the calc-alkaline magmas.
Xenoliths found below an autochthonous pumice layer prove penetration of
granites, phyllites and limestone by the rising magma. The geochemical investigations
support a subduction type origin of the volcanic material of the Christiana
Islands