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• Barnichon J.-D., Havenith H.B., Hoffer B., Charlier R., Jongmans D., Duchesne J.C. The deformation of the Egersund-Ogna massif, South Norway: finite element modelling of diapirism. Tectonophysics 1999, 303:109-130.
• Bingen B., van Breemen O. Tectonic regimes and terrane boundaries in the high-grade Sveconorwegian belt of SW Norway, inferred from U-Pb zircon geochronology and geochemical signature of augen gneiss suites. J. Geol. Soc. (Lond.) 1998, 155:143-154.
• Bingen B., Demaiffe D., Hertogen J., Weis D., Michot J. K-rich calc-alkaline augen gneisses of Grenvillian age in SW Norway: mingling of mantle-derived and crustal components. J. Geol. 1993, 101:763-778.
• Bybee G.M., Ashwal L.D., Shirey S.B., Horan M., Mock T., Andersen T.B. Pyroxene megacrysts in Proterozoic anorthosites: implications for tectonic setting, magma source and magmatic processes at the Moho. Earth Planet. Sci. Lett. 2014, 389:74-85.
• Charlier B., Duchesne J.C., Vander Auwera J., Storme J., Maquil R., Longhi J. Polybaric fractional crystallization of high-alumina basalt parental magmas in the Egersund-Ogna massif-type anorthosite (Rogaland, SW Norway) constrained by plagioclase and high-alumina orthopyroxene megacrysts. J. Petrol. 2010, 51:2515-2546.
• Drüppel K., Elsäber L., Brandt S., Gerdes A. Sveconorwegian mid-crustal ultrahigh-temperature metamorphism in Rogaland, Norway: U-Pb LA-ICP-MS geochronology and pseudosections of sapphirine granulites and associated paragneisses. J. Petrol. 2013, 54:305-350.
• Duchesne J.C., Liégeois J.P., Vander Auwera J., Longhi J. The crustal tongue melting model and the origin of massive anorthosites. Terra Nova 1999, 11:100-105.
• Emslie R.F. Ages and petrogenetic significance of igneous mangerite-charnockite suites associated with massif anorthosites, Grenville Province. J. Geol. 1990, 98:213-231.
• Fram M., Longhi J. Phase equilibria of dikes associated with Proterozoic anorthosite complexes. Am. J. Sci. 1992, 77:605-616.
• Hamilton M., Ryan A., Emslie R., Ernanovics I. Identification of Paleoproterozoic anorthositic and monzonitic rocks in the vicinity of the Mesoproterozoic Nain Plutonic Suite, Labrador: U-Pb evidence 1998, 23-40. Radiogenic Age and Isotopic Studies. Geological Survey of Canada, Report 11, current research 1998-F.
• Hermann J., Müntener O., Günther D. Differentiation of mafic magma in a continental crust-to-mantle transition zone. J. Petrol. 2001, 42:189-206.
• Longhi J., Vander Auwera J., Fram M., Duchesne J.C. Some phase equilibrium constraints on the origin of Proterozoic (massif) anorthosites and related rocks. J. Petrol. 1999, 40:339-362.
• Müntener O., Kelemen P., Grove T. The role of H2O during crystallization of primitive arc magmas under uppermost mantle conditions and genesis of igneous pyroxenites: an experimental study. Contrib. Mineral. Petrol. 2001, 141:643-658.
• Myers J., Voordouw R., Tettelaar T. Proterozoic anorthosite-granite Nain batholith: structure and intrusion processes in an active lithosphere-scale fault zone, northern Labrador. Can. J. Earth Sci. 2008, 45:909-934.
• Ryan B., Hamilton M., Emslie R., Connelly J. Paleoproterozoic and Mesoproterozoic anorthositic and granitic plutons in the Nain-Okak region, Labrador: repetitive anorogenic magmatism. Eos 1999, S366.
• Schärer U., Wilmart E., Duchesne J.C. The short duration and anorogenic character of anorthosite magmatism: U-Pb dating of the Rogaland complex, Norway. Earth Planet. Sci. Lett. 1996, 139:335-350.
• Vander Auwera J., Bolle O., Bingen B., Liégeois J.-P., Bogaerts B., Duchesne J.C., De Waele B., Longhi J. Sveconorwegian massif-type anorthosites and related granitoids result from post-collisional melting of a continental arc root. Earth-Sci. Rev. 2011, 107:375-397.
• Weis D. Genetic implications of Pb isotope geochemistry in the Rogaland anorthositic complex (southwest Norway). Chem. Geol. 1986, 57:181-199.