Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6443816 | Journal of African Earth Sciences | 2014 | 58 Pages |
Abstract
Large idiomorphic zircon crystals (megacrysts), found in the vicinity of the carbonatite can directly be related to the carbonatite evolution. They have been dated at 705.5 ± 4.5 Ma (U-Pb concordant age, LA-ICP-MS). Similar zircon megacrysts of the Lueshe carbonatite (DRCongo) have been dated and give a concordant age at 798.5 ± 4.9 Ma (U-Pb, LA-ICP-MS). Considering that an extensional tectonic regime occured at that time in Central Africa - what remains debated - both ages could relate to different stages of Rodinia breakup, with uprise of mantle-derived magmas along Palaeoproterozoic lithospheric zones of weakness.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Gilbert Midende, Philippe Boulvais, Luc Tack, Frank Melcher, Axel Gerdes, Stijn Dewaele, Daniel Demaiffe, Sophie Decrée,