3 resultater
The project has documented the existence of several previously unknown platinum group element (PGE) mineralizations in Norwegian ophiolites, of a type previously not well-documented anywhere, i.e. stratiform platinum- palladium-gold mineralization in ultramafic cumulates in ophiolites. PGE- bearing podiform chromitite and high level Ni-Cu sulphide mineralizations have also been studied.
Primary and re-equilibrated mineral assemblages from the Sveconorwegian mafic intrusions of the Kongsberg ...
... P. Kutyavin, Andrei V. Sochava Page(s): 24-25 Heavy mineral assemblages in the Neoproterozoic rocks of the Varanger Peninsula, ... B. Larsen, Mogens Marker Page(s): 34-35 Ilmenite mineral magnetism: implications for geophysical exploration for ilmenite ...
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