PGE reefs as an in situ crystallization phenomenon: the Nadezhda gabbronorite body, Lukkulaisvaara layered intrusion, Fennoscandian Shield, Russia

Summary The 100 m thick and 700 m long Nadezhda sill-like gabbronorite body, emplaced in the mafic-ultramafic Lukkulaisvaara layered intrusion, is associated with Cu-Ni-PGE mineralization that is mostly confined to mottled anorthosites developed from host gabbronorites and norites along the margin o...

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Veröffentlicht in:	Mineralogy and petrology 2008, Vol.92 (1-2), p.211-242
Hauptverfasser:	Latypov, R. M., Chistyakova, S. Yu, Alapieti, T. T.
Format:	Artikel
Sprache:	eng
Schlagworte:	Crystallization Earth and Environmental Science Earth Sciences Geochemistry Geology Inorganic Chemistry Magma Mineralization Mineralogy Petrology Sulfides
Online-Zugang:	Volltext
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