The norite-mangerite relationships in the Bjerkreim-Sokndal layered lopolith (southwest Norway)
References (48)
- et al.
Trace element variations and isotopic composition of charnockitic acidic rocks related to anorthosites (Rogaland — S.W. Norway)
- et al.
Trace elements and anorthosite genesis
Earth Planet. Sci. Lett.
(1978) Anorthosite massifs, rapakivi granites, and Late Proterozoic rifting of North America
Precambrian Res.
(1978)Liquid immiscibility in alkali-rich magmas
Chem. Geol.
(1978)- et al.
Instrumental neutron activation analysis of rocks with a low-energy photon detector
Anal. Chem. Acta
(1971) - et al.
UPb and RbSr geochronology of the eastern part of the South Rogaland igneous complex, Southern Norway
Lithos
(1979) - et al.
Implications of liquid-liquid distribution coefficients to mineral-liquid partitioning
Geochim. Cosmochim. Acta
(1978) Commingling of magmas in the Bjerkrem-Sogndal lopolith (southwest Norway): evidence for the compositions of residual liquids
Lithos
(1984)- et al.
The viscosity of magmatic silicate liquids, a model for calculation
Am. J. Sci.
(1972) Differentiation trends and parental magmas for anorthositic and quartz mangerite series, Adirondacks, New York
Geol. Soc. Am. Mem.
(1972)
Iron-titanium oxide minerals and synthetic equivalents
J. Petrol.
Plagioclase buoyancy in basaltic liquids as determined with a centrifuge furnace
Contrib. Mineral. Petrol.
Microtextures of FeTi oxide minerals in the South-Rogaland anorthositic complex (Norway)
Ann. Soc. Géol. Belg.
Iron-titanium oxide minerals in the Bjerkrem-Sogndal massif, southwestern Norway
J. Petrol.
Pyroxènes et olivines dans le massif de Bjerkrem-Sogndal (Norvège méridionale). Contribution à l'étude de la série anorthosite-mangérite
Quantitative modeling of Sr, Ca, Rb and K in the Bjerkrem-Sogndal layered lopolith (S.W. Norway)
Contrib. Mineral. Petrol.
The Rogaland anorthosites: facts and speculations
The high-grade metamorphic Precambrian of the Sirdal-Örsdal area, Rogaland/Vest-Agder, S.W. Norway
Nor. Geol. Unders.
Double-diffusive convection due to crystallization in magmas
Annu. Rev. Earth Planet. Sci.
Terminology for layered intrusions
J. Petrol.
FeTi mineralizations in the Åna-Sira anorthosite, southern Norway
Viscosity, density, and structure of silicate melts at high pressure, and their petrological applications
L'évolution magmatique du complexe de Morin et son apport au problème des anorthosites
Contrib. Mineral. Petrol.
Differentiation of the Skaergaard intrusion
Nature (London)
Cited by (28)
The origin of nelsonite and high-Zr ferrodiorite associated with Proterozoic anorthosite
2015, Ore Geology ReviewsCitation Excerpt :Whereas the Si-rich melt conjugate with rock #78-32-2 (margin of the Tellnes dyke) approached a quartz mangeritic composition, the Si-rich melts associated with the primitive high-Zr jotunites are not known. It has been suggested that some quartz mangerite from the upper part of the BKSK intrusion could represent immiscible melts on top of the layered series (Wilson and Overgaard, 2005) despite objections raised by Duchesne et al. (1987) and Duchesne and Wilmart (1997). More work on trace element on apatite and zircon compositions in acidic rocks is needed to solve this issue.
Fe-Ti-V-P ore deposits associated with Proterozoic massif-type anorthosites and related rocks
2015, Earth-Science ReviewsCitation Excerpt :However, the magnetite may represent a significant source of V, so the economic potential has to be evaluated, especially when combined with Ti from ilmenite and P from apatite (Fig. 7). Examples of this ore type are present in the Magpie Mountain (Lac St Jean anorthosite, Québec; Perreault, 2003), the Suwalki anorthosite (NE Poland; Charlier et al., 2009), the Fedorivka layered intrusion (Korosten Complex, Ukraine; Duchesne et al., 2006), the Krapivnia deposit (Korosten Complex, Ukraine; Gursky et al., 2003) and in the Transition Zone of the Bjerkreim–Sokndal layered intrusion (Duchesne et al., 1987). Nelsonites are Fe–Ti-oxide-apatite rocks (Fig. 8).