Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4729185 | Journal of African Earth Sciences | 2011 | 20 Pages |
Abstract
⺠The studied region lies across the western boundary of the Saharan metacraton. ⺠Eastern basement protolith is dated at 1918±Ma and gneissification at 580±26 Ma. ⺠AMS fabric of the Eburnean granitic gneiss is related to the Pan-African tectonics. ⺠Pan-African granites are dated at 595±3 Ma and 582±3 Ma. ⺠AMS fabric is late-magmatic in most Pan-African plutons.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
O. Nouar, B. Henry, J.P. Liégeois, M.E.M. Derder, B. Bayou, O. Bruguier, A. Ouabadi, M. Amenna, A. Hemmi, M. Ayache,