Abstract
Large magnesian ilmenite “nodules” occur in a quaternary basanitic volcano near Silet in the Tahalra volcanic area (Central Ahaggar, Southern Algeria). Their texture, from foliated to polygonal, is ascribed to solid state flow and dynamic recrystallization in upper mantle conditions.
Their composition is similar to that of kimberlitic Mg-ilmenite nodules, as regards Mg, Fe, Al and Cr contents; the geikielite content ranges from 25 to 37 mol %. No outwards Mg enrichment of the nodules has been observed. Peripheral secundary products (pseudobrookite, magnetite and hematite) result from reaction with the host magma.
From textural relationships and microprobe analyses, the Mg-ilmenite nodules from Tahalra are thought to be early cumulates from a mafic melt fractionnated in the upper-mantle; later, after solid-state deformation, these ilmenitite rocks were sampled and carried up to the surface by a fast-rising basanitic liquid.
Rocks almost exclusively made of ilmenite do therefore presently exist within the upper-mantle and form a new type of petrological heterogeneity.
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Leblanc, M., Dautria, J.M. & Girod, M. Magnesian ilmenitite xenoliths in a basanite from Tahalra, Ahaggar (Southern Algeria). Contr. Mineral. and Petrol. 79, 347–354 (1982). https://doi.org/10.1007/BF01132063
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DOI: https://doi.org/10.1007/BF01132063