Physics
Scientist
Isotope Geology, Royal Museum for Central Africa, Tervuren, Belgium
Anorthosite formation by plagioclase flotation in ferrobasalt and implications for the lunar crust
Sveconorwegian massif-type anorthosites and related granitoids result from post-collisional melting of a continental arc root
Sveconorwegian massif-type anorthosites and related granitoids result from post-collisional melting of a continental arc root
Tadhak alkaline ring-complex (Mali): existence of U-Pb isochrons and ``Dupal'' signature 270 Ma ago
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