1. Barbey, P. (1986). Signification géodynamique des domaines granulitiques. La ceinture des granulites de Laponie (Fennoscandie): une suture de collision continentale d’âge protérozoique inférieur (2.3–1.9 Ga). Mém. Docum. Centre Arm. Et. Struct. Socles, Rennes, 7: 346p.
2. Barbey, P. and Cuney, M. (1982). Rb, Sr, Ba, U and Th geochemistry of the Lapland granulites. Contrib. Mineral. Petrol., 81: 304–316.
3. Barbey, P., Convert, J., Martin, H., Moreau, B., Capdevila, R. and Hameurt, J. (1980). Relationships between granite-gneiss terrains, greenstone belts and granulite belts in the Archaean crust of Lapland (Fennoscandia). Geol. Rundschau, 69: 648–658.
4. Barbey, P., Capdevila, R. and Hameurt, J. (1982). Major and transition trace element abundances in the khondalite suite of the Granulite belt of Lapland (Fennoscandia). Evidence for an early Proterozoic flysch-belt. Precambrian Res., 16: 273–290.
5. Barbey, P., Convert, J., Moreau, B., Capdevila, R. and Hameurt, J. (1984). Pedogenesis and evolution of an early Proterozoic collisional orogenic belt: the Granulite belt of Lapland and the Belomorides (Fennoscandia). Bull. Geol. Surv. Finland, 56: 161–188.