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

Journal of Petrology

Volumn 51, Issue 12, 2010, Pages 2515-2546

  Charlier, B ^a   Duchesne, J C ^a   Vander Auwera, J ^a   Storme, J Y ^a   Maquil, R ^b   Longhi, J ^c  

^a UNIVERSITY OF LIÈGE   (Belgium)

^b Geological Survey of Grand Duchy of Luxembourg   (Luxembourg)

^c Doherty Earth Observatory of Columbia University   (United States)

Author keywords

AMCG; Diapir; Emplacement mechanism; Partition coefficients; Proterozoic; Trace element modelling

Indexed keywords

ALUMINUM OXIDE; ANORTHOSITE; BASALT; CONCENTRATION (COMPOSITION); CRYSTALLIZATION; DIAPIR; EMPLACEMENT; EXPERIMENTAL MINERALOGY; FRACTIONAL CRYSTALLIZATION; MAGMA; MAGMATIC DIFFERENTIATION; MEGACRYST; ORTHOPYROXENE; PARENT BODY; PARTITION COEFFICIENT; PLAGIOCLASE; PLUTON; PRESSURE EFFECT; PROTEROZOIC;

EGERSUND; NORWAY; OGNA; ROGALAND;

EID: 78649850793     PISSN: 00223530     EISSN: 14602415     Source Type: Journal    
DOI: 10.1093/petrology/egq066     Document Type: Article

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