Petrogenesis of monzonoritic dykes in the Egersund-Ogna anorthosite (Rogaland, S.W. Norway): trace elements and isotopic (Sr, Pb) constraints

Author:

Duchesne J. C.,Roelandts I.,Demaiffe D.,Weis D.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference38 articles.

1. Ashwal LD (1982) Mineralogy of mafic and Fe-Ti oxide rich differentiates of the Marcy anorthosite massif, Adirondacks, New York. Am Mineral 67:14–27

2. Othman Othman D, Polvé M, Allègre CJ (1984) Nd-Sr composition of granulites. Constraints on the evolution of the lower conental crust. Nature 307:510–515

3. Buddington AF (1972) Differentiation trends and parental magmas for anorthositic and quartz mangerite series, Adirondacks, New-York. Geol Soc Am Mem 132:477–488

4. Demaiffe D (1977) De l'origine des anorthosites. Pétrologie, géochimie et géochimie isotopique des massifs anorthositiques de Hidra et de Garsaknatt (Rogaland, Norvège méridionale). Unpubl Dr Sc Thesis, Univ Bruxelles

5. Demaiffe D, Hertogen J (1981) Rare earth geochemistry and strontium isotopic composition of a massif-type anorthositic-charnockitic body: the Hidra massif (Rogaland, S.W. Norway). Geochim Cosmochim Acta 45:1545–1561

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