Abstract In the Veria-Naousa ophiolitic complex (north Greece), rodingite appears mainly in
the form of cross cutting dykes within serpentinised peridotites. It is distinguished into three
types, based upon the provenance of its protoliths, textural characteristics, mineralogical
assemblages and geochemical affinities. Type I rodigites were derived from boninitic
diabasic protoliths and their mineralogical assemblage include garnet+ clinopyroxene+
chlorite. Type II rodingites were formed at the expense of gabbroic precursors, comprising …