“…Flow-alignment of alkali feldspar, albite and aegirine phenocrysts imparts a foliated trachytic texture ( Fig. 2a), identical to that of type-locality lujavrite at Lovozero (Ramsay, 1890;Féménias et al, 2005). All of the 'green foyaites' which consist of alkali feldspar, albite, nepheline, sodalite, aegirine, eudialyte and sodic amphibole as primary minerals, are termed lujavrite in this work, regardless of their texture.…”