Daniel Demaiffe
Université libre de Bruxelles
162 Papers
1.6K Citations
Daniel Demaiffe is an academic researcher from Université libre de Bruxelles. The author has contributed to research in topics: Massif & Fractional crystallization (geology). The author has an hindex of 39, co-authored 161 publications. Previous affiliations of Daniel Demaiffe include University of La Rochelle.
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Papers
The Cameroon Hot Line (CHL): A unique example of active alkaline intraplate structure in both oceanic and continental lithospheres
TL;DR: The Cameroon Hot Line (CHL) is an active N30°E tectono-magmatic alignment, extending from Pagalu Island to Lake Chad as discussed by the authors, and is composed of six major volcanoes, numerous monogenic cones and more than sixty plutonic anorogenic ring complexes.
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Redistribution of rare earth elements, thorium, and uranium over accessory minerals in the course of amphibolite to granulite facies metamorphism: The role of apatite and monazite in orthogneisses from southwestern Norway
TL;DR: The amphibolite to granulite facies transition has been studied in a high-K calc-alkaline, hornblende-biotite, K-feldspar megacrystic augen gneiss series from the Rogaland-Vest-Agder (Rog-VA) sector of the Sveconorwegian province (southwest Norway).
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Petrogenesis of Neoproterozoic Granitoids and Related Rocks from the Seychelles: the Case for an Andean-type Arc Origin
TL;DR: The Seychelles islands consist of undeformed and unmetamorphosed basaltic magmas derived from metaluminous monzogranites and granodiorites of Neoproterozoic depleted mantle, variably contaminated by Archaean age (> 750 Ma.
200
The 616 Ma Old Egersund Basaltic Dike Swarm, Sw Norway, and Late Neoproterozoic Opening of the Iapetus Ocean
TL;DR: The Egersund dike swarm of SW Norway is made up of 11 basaltic dikes trending ESE•WNW and has a U-Pb intrusive age of 616 ± 3 Ma as mentioned in this paper.
192
Petrogenetic processes in the ultramafic, alkaline and carbonatitic magmatism in the Kola Alkaline Province: A review
TL;DR: In this article, the authors classified the Devonian Kola Alkaline Carbonatite Province (KACP) into four groups: (a) primitive mantle-derived silica-under saturated silicate magmas; (b) evolved alkaline and nepheline syenites; (c) cumulate rocks; (d) carbonatites and phoscorites, some of which may also be cumulates.
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