| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 5785623 | Journal of African Earth Sciences | 2017 | 40 Pages |
Abstract
Three generations of Eburnean granitoids are recognized: (i) early (2215-2160Â Ma); (ii) syn-tectonics (2150-2100Â Ma) and post-tectonics (2090-2040Â Ma). The lithological succession, geochemical and metamorphic characteristics of these units point to an ophiolitic supra-subduction zone.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Moussa Dabo, Tahar Aïfa, Ibrahima Gning, Malick Faye, Mamadou Fallou Ba, Papa Malick Ngom,