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-Reference-Cited by-同舟云学术

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

Published:2010-11-23 Issue:12 Volume:51 Page:2515-2546
ISSN:1460-2415
Container-title:Journal of Petrology
language:en
Short-container-title:

Author:

Charlier B.,Duchesne J.-C.,Vander Auwera J.,Storme J.-Y.,Maquil R.,Longhi J.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/petrology/article-pdf/51/12/2515/16672384/egq066.pdf

Reference63 articles.

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3. Anorthosites

4. The deformation of the Egersund Ogna massif, South Norway: Finite element modelling of diapirism;Barnichon;Tectonophysics,1999

5. Parental magmas of the Nain plutonic suite anorthosites and mafic cumulates: a trace element modelling approach;Bédard;Contributions to Mineralogy and Petrology,2001

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