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4.2 Field Citation Ratio

n/a Relative Citation Ratio

• Aigner-Torres, M., Blundy, J., Ulmer, P. & Pettke, T. (2007). Laser ablation ICPMS study of trace element partitioning between plagioclase and basaltic melts: an experimental approach. Contributions to Mineralogy and Petrology 153, 647-667.
• Anderson, A. T. & Morin, M. (1969). Two types of massif anorthosite and their implications regarding the thermal history of the crust. In: Isachsen, Y. W. (ed.) Origin of Anorthosite and Related Rocks. New York State Museum and Science Service Memoir 18, 57-69.
• Ashwal, L. D. (1993). Anorthosites. Heidelberg: Springer, 422 p.
• Barnichon, J.-D., Havenith, H., Hoffer, B., Charlier, R., Jongmans, D. & Duchesne, J. C. (1999). The deformation of the Egersund Ogna massif, South Norway: Finite element modelling of diapirism. Tectonophysics 303, 109-130.
• Beédard, J. H. (2001). Parental magmas of the Nain plutonic suite anorthosites and mafic cumulates: a trace element modelling approach. Contributions to Mineralogy and Petrology 141, 747-771.
• Berg, J. H. (1977). Dry granulite mineral assemblages in the contact aureoles of the Nain complex, Labrador. Contributions to Mineralogy and Petrology 64, 33-52.
• Bindeman, I. N., Davis, A. M. & Drake, M. J. (1998). Ion microprobe study of plagioclase-basalt partition experiments at natural concentration levels of trace elements. Geochimica et Cosmochimica Acta 62, 1175-1193.
• Bingen, B., Demaiffe, D. & van Breemen, O. (1998). The 616-My-old Egersund basaltic dike swarm, SW Norway, and the late Proterozoic opening of the Iapetus Ocean. Journal of Geology 106, 565-574.
• Blundy, J. D. & Wood, B. J. (1991). Crystal-chemical controls on the partitioning of Sr and Ba between plagioclase feldspar, silicate melts, and hydrothermal solutions. Geochimica et Cosmochimica Acta 55, 193-209.
• Bogdanova, S. V., Pashkevich, I. K., Buryanov, V. B., Makarenko, I. B., Orlyuk, M. I., Skobelev, V. M., Starostenko, V. I. & Legostaeva, O. V. (2004). The 1.80-1.74-Ga gabbro-anorthosite-rapakivi Korosten Pluton in the Ukrainian Shield: a 3-D geophysical reconstruction of deep structure. Tectonophysics 381, 5-27.
• Corrigan, D. & Hanmer, S. (1997). Anorthosites and related granitoids in the Grenville orogen: a product of convective thinning of the lithosphere? Geology 25, 61-64.
• Demaiffe, D. & Hertogen, J. (1981). Rare earth element geochemistry and strontium isotopic composition of a massif-type anorthositic-charnockitic body: the Hidra massif (Rogaland, SW Norway). Geochimica et Cosmochimica Acta 45, 1545-1561.
• Duchesne, J. C. & Demaiffe, D. (1978).Trace elements and anorthosite genesis. Earth and Planetary Science Letters 38, 249-272.
• Duchesne, J. C. & Hertogen, J. (1988). Le magma parental du lopolithe de Bjerkreim-Sokndal (Norvège meéridionale). Comptes Rendus de l'Acadeémie des Sciences 306, 45-48.
• Duchesne, J. C. & Korneliussen, A. (eds) (2003). Ilmenite deposits and their geological environment, with special reference to the Rogaland Anorthosite Province, including a geological map at scale 1:75,000 and a CD with a guide to the province. Norges Geologiske Undersøkelse Special Publication 9, 138 p.
• Duchesne, J. C. & Maquil, R. (1987). The Egersund-Ogna massif. In: Maijer, C. & Padget, P. (eds) The Geology of Southernmost Norway: an excursion guide. Norges Geologiske Undersøkelse Special Publication 1, 50-56.
• Duchesne, J. C., Roelandts, I., Demaiffe, D. & Weis, D. (1985a). Petrogenesis of monzonoritic dykes in the Egersund-Ogna anorthosite (Rogaland, S.W. Norway): trace elements and isotopic (Sr, Pb) constraints. Contributions to Mineralogy and Petrology 90, 214-225.
• Duchesne, J. C., Maquil, R. & Demaiffe, D. (1985b). The Rogaland anorthosites: facts and speculations. In: Tobi, A. C. & Touret, J. L. R. (eds) The Deep Proterozoic Crust in the North Atlantic Province. Dordrecht: Reidel, pp. 449-476.
• Duchesne, J. C., Lieégeois, J. P.,Vander Auwera, J. & Longhi, J. (1999). The crustal tongue melting model and the origin of massive anorthosites. Terra Nova 11, 100-105.
• Dymek, R. F. (2004). Anorthosite magma revisited: field and petrographic evidence from the CRUML belt, Grenville Province, Quebec. EOS Transactions of the American Geophysical Union 85(17), Joint Assembly Supplement JA513, Abstract V51E-01.
• Dymek, R. F. & Gromet, L. P. (1984). Nature and origin of orthopyroxene megacrysts from the St-Urbain anorthositic massif, Quebec. Canadian Mineralogist 22, 297-326.
• Emslie, R. F. (1975). Pyroxene megacrysts from anorthositic rocks: a new clue to the sources and evolution of the parent magmas. Canadian Mineralogist 13, 138-145.
• Emslie, R. F. (1980). Geology and petrology of the Harp Lake Complex, central Labrador: an example of Elsonian magmatism. Geological Survey of Canada Bulletin 293, 1-136.
• Emslie, R. F. (1985). Proterozoic anorthosite massifs. In: Tobi, A. C. & Touret, J. L. R. (eds) The Deep Proterozoic Crust in the North Atlantic Provinces. Dordrecht: Reidel, pp. 39-60.
• Emslie, R. F. (1991). Granitoids of rapakivi granite-anorthosite and related associations. Precambrian Research 51, 173-192.
• Emslie, R. F., Hamilton, M. A. & Theriault, R. J. (1994). Petrogenesis of a Midproterozoic anorthosite-mangerite-charnockite-granite (AMCG) complex-isotopic and chemical evidence from the Nain Plutonic Suite. Journal of Geology 120, 539-558.
• Fram,M. & Longhi, J. (1992). Phase equilibria of dikes associated with Proterozoic anorthosite complexes. AmericanMineralogist 77,605-616.
• Ghiorso, M. S. & Sack, R. O. (1995). Chemical mass transfer in magmatic processes IV. A revised and internally consistent thermodynamic model for the interpolation and extrapolation of liquid-solid equilibria in magmatic systems at elevated temperatures and pressures. Contributions to Mineralogy and Petrology 119, 197-212.
• Jansen, J. B. H., Blok, R. J. P., Bos, A. & Scheelings, M. (1985). Geothermometry and geobarometry in Rogaland and preliminary results from the Bamble area. In: Tobi, A. C. & Touret, J. L. R. (eds) The Deep Proterozoic Crust in the North Atlantic Provinces. Dordrecht: Reidel, pp. 499-516.
• Kushiro, I. & Fujii, T. (1977). Flotation of plagioclase in magma at high pressures and its bearing on the origin of anorthosite. Proceedings of theJapan Academy, Series B 53, 262-266.
• Lafrance, B., John, B. E. & Scoates, J. S. (1996). Syn-emplacement recrystallization and deformation microstructures in the Poe Mountain anorthosite, Wyoming. Contributions to Mineralogy and Petrology 122, 431-440.
• Lindsley, D. H. (1969). Melting relations of plagioclase at high pressures. In: Isachsen,Y.W. (ed.) Origin of Anorthosite and Related Rocks. NewYork State Museum and Science Service Memoir 18, 39-46.
• Longhi, J. (2005). A mantle or mafic crustal source for Proterozoic anorthosites? Lithos 83, 183-198.
• Longhi, J. & Ashwal, L. D. (1985). Two-stage models for lunar and terrestrial anorthosites: petrogenesis without a magma ocean. Proceedings of the 15th Lunar and Planetary Science Conference, Part 2. Journal of Geophysical Research 90(Supplement): C571-C584.
• Longhi, J., Vander Auwera, J., Fram, M. & Monthieth, J. N. (1993). Pressure effects, kinetics and rheology of anorthositic and related magmas. American Mineralogist 78, 1016-1030.
• Longhi, J.,Vander Auwera, J., Fram, M. S. & Duchesne, J. C. (1999). Some phase equilibrium constraints on the origin of Proterozoic (massif) anorthosites and related rocks. Journal of Petrology 40, 339-362.
• Maquil, R. & Duchesne, J. C. (1984). Geéothermomeétrie par les pyroxènes et mise en place du massif anorthositique d'Egersund-Ogna (Rogaland, Norvège meéridionale). Annales de la Socieéteé Geéologique de Belgique 107, 27-49.
• Marker, M., Schiellerup, H., Meyer, G. B., Robins, B. & Bolle, O. (2003). Geological map of the Rogaland anorthosite province-scale 1:75000. In: Duchesne, J. C. & Korneliussen, A. (eds) Ilmenite deposits and their geological environment. With special reference to the Rogaland Anorthosite Province. Norges Geologiske Undersøkelse Special Publication 9, Plate1.
• Martignole, J. & Schrijver, K. (1970). Tectonic significance and evolution of the Morin anorthosite, Grenville Province, Quebec. Bulletin of the Geological Society of Finland 42, 165-209.
• Michot, J. & Michot, P. (1969). The problem of anorthosites: the South Rogaland igneous complex, southern Norway. In: Isachsen, Y. W. (ed.) Origin of Anorthosite and Related Rocks. New York State Museum Sciences Service Memoir 18, 399-410.
• Mitchell, J. N., Scoates, J. S. & Frost, C. D. (1995). High-Al gabbros in the Laramie anorthosite complex, Wyoming-Implications for the composition of melts parental to Proterozoic anorthosite. Contributions to Mineralogy and Petrology 119, 166-180.
• Morse, S. A. (1975). Plagioclase lamellae in hypersthene, Tikkoatokhakh Bay, Labrador. Earth and Planetary Science Letters 26, 331-336.
• Morse, S. A. (2006). Labrador massif anorthosites: Chasing the liquids and their sources. Lithos 89, 202-221.
• Morse, S. A. (2008). The internal magma reservoir of large intrusions revealed by multiphase Rayleigh fractionation. Journal of Petrology 49, 2081-2098.
• Myers, J. S.,Voordouw, R. J. & Tettelaar,T. A. (2008). Proterozoic anorthosite-granite Nain batholith: structure and intrusion processes in an active lithosphere-scale fault zone, northern Labrador. Canadian Journal of Earth Sciences 45, 909-934.
• Owens, B. E. & Dymek, R. F. (1995). Significance of pyroxene megacrysts for massif anorthosite petrogenesis: Constraints from the Labrieville, Quebec, pluton. American Mineralogist 80, 144-161.
• Owens, B. E. & Dymek, R. F. (2005). Rediscovery of the Mattawa anorthosite massif, Grenville Province, Quebec. Canadian Journal of Earth Sciences 42, 1699-1718.
• Putirka, K. A. (2005). Igneous thermometers and barometers based on plagioclase plus liquid equilibria: Tests of some existing models and new calibrations. American Mineralogist 90, 336-346.
• Robins, B., Tumyr, O., Tysseland, M. & Garman, L. D. (1997). The Bjerkreim-Sokndal layered intrusion, Rogaland, SW Norway: evidence from marginal rocks for a jotunite parent magma. Lithos 39, 121-133.
• Ryan, B. (2000). The Nain-Churchill boundary and the Nain Plutonic Suite: a regional perspective on the geologic setting of theVoisey's Bay Ni-Cu-Co deposit. Economic Geology 95, 703-724.
• Schärer, U., Wilmart, E. & Duchesne, J. C. (1996). The short duration and anorogenic character of anorthosite magmatism: U-Pb dating of the Rogaland complex, Norway. Earth and Planetary Science Letters 139, 335-350.
• Schiellerup, H., Korneliussen, A., Heldal, T., Marker, M., Bjerkgård, T. & Nilsson, L.-P. (2003). Mineral resources in the Rogaland Anorthosite Province, South Norway: origins, history and recent developments. In: Duchesne, J. C. & Korneliussen, A. (eds) Ilmenite deposits and their geological environment. With special reference to the Rogaland Anorthosite Province. Norges Geologiske Undersøkelse Special Publication 9, 116-134.
• Scoates, J. S. & Chamberlain, K. R. (1997). Orogenic to post-orogenic origin for the 1.76 Ga Horse Creek anorthosite complex, Wyoming, USA. Journal of Geology 105, 331-343.
• Smith, J. V. & Ribbe, P. H. (1969). Atomic movements in plagioclase feldspars: Kinetic interpretation. Contributions to Mineralogy and Petrology 21, 157-202.
• Smithson, S. B. & Ramberg, I. B. (1979). Gravity interpretation of the Egersund anorthosite complex, Norway: Its petrological and geothermal significance. Geological Society of America Bulletin 90, 199-204.
• Toplis, M. J. & Corgne, A. (2002). An experimental study of element partitioning between magnetite, clinopyroxene and iron-bearing silicate liquids with particular emphasis on vanadium. Contributions to Mineralogy and Petrology 144, 22-37.
• Vander Auwera, J. & Longhi, J. (1994). Experimental study of a jotunite (hypersthene monzodiorite): constraints on the parent magma composition and crystallization conditions (P, T, fO2) of the Bjerkreim-Sokndal layered intrusion (Norway). Contributions to Mineralogy and Petrology 118, 60-78.
• Vander Auwera, J., Longhi, J. & Duchesne, J. C. (1998). A liquid line of descent of the jotunite (hypersthene monzodiorite) suite. Journal of Petrology 39, 439-468.
• Vander Auwera, J., Longhi, J. & Duchesne, J. C. (2000). The effect of pressure on DSr (plag/melt) and DCr (opx/melt): implications for anorthosite petrogenesis. Earth and Planetary Science Letters 178, 303-314.
• Westphal, M., Schumacher, J. C. & Boschert, S. (2003). Hightemperature metamorphism and the role of magmatic heat sources at the Rogaland Anorthosite Complex in Southwestern Norway. Journal of Petrology 44, 1145-1162.
• Wiebe, R. A. (1992). Proterozoic anorthosite complexes. In: Condie, K. C. (ed.) Proterozoic Crustal Evolution. Amsterdam: Elsevier, pp. 215-262.
• Wilmart, E. & Duchesne, J. C. (1987). Geothermobarometry of igneous and metamorphic rocks around the Ana-Sira anorthosite massif: implications for the depth of emplacement of the South Norwegian anorthosites. Norsk Geologisk Tidsskrift 67, 185-196.
• Xue, S. & Morse, S. A. (1994). Chemical characteristics of plagioclase and pyroxene megacrysts and their significance to the petrogenesis of the Nain anorthosites. Geochimica et Cosmochimica Acta 58, 4317-4331.