Origin of Cretaceous alkaline annular structures in the peri
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Ihouhaouene carbonatites and associated syenites in total
The “eye of Africa” (Richat dome, Mauritania): An isolated
Comparison between igneous (left) and sedimentary (right
Light rare earth element redistribution during hydrothermal
B-Incompatible elements normalized to the primitive mantle
Covariation diagrams of Fo versus NiO (a), CaO (b), MnO (c
Spydergrams of phoscorite (1A) and carbonatite (1C).
Cathodoluminescence images of zircons recovered from the
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Clinopyroxene mineral chemistry of the Ihouhaouene carbonatites
Origin of Cretaceous alkaline annular structures in the peri
Thorium-poor monazite and columbite-(Fe) mineralization in the
Carbonate sedimentary textures in PPL (left) and
Origin of Cretaceous alkaline annular structures in the peri
Comparison between igneous and sedimentary limestones texture. (a
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