Leblanc, M., Lancelot, J. R. (1980) Interprétation géodynamique du domaine pan-africain (Précambrien terminal) de l'Anti-Atlas (Maroc) à partir de données géologiques et géochronologiques. Canadian Journal of Earth Sciences, 17 (1) 142-155 doi:10.1139/e80-012
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Interprétation géodynamique du domaine pan-africain (Précambrien terminal) de l'Anti-Atlas (Maroc) à partir de données géologiques et géochronologiques | ||
| Journal | Canadian Journal of Earth Sciences | ||
| Authors | Leblanc, M. | Author | |
| Lancelot, J. R. | Author | ||
| Year | 1980 (January 1) | Volume | 17 |
| Issue | 1 | ||
| Publisher | Canadian Science Publishing | ||
| DOI | doi:10.1139/e80-012Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 476489 | Long-form Identifier | mindat:1:5:476489:6 |
| GUID | 0 | ||
| Full Reference | Leblanc, M., Lancelot, J. R. (1980) Interprétation géodynamique du domaine pan-africain (Précambrien terminal) de l'Anti-Atlas (Maroc) à partir de données géologiques et géochronologiques. Canadian Journal of Earth Sciences, 17 (1) 142-155 doi:10.1139/e80-012 | ||
| Plain Text | Leblanc, M., Lancelot, J. R. (1980) Interprétation géodynamique du domaine pan-africain (Précambrien terminal) de l'Anti-Atlas (Maroc) à partir de données géologiques et géochronologiques. Canadian Journal of Earth Sciences, 17 (1) 142-155 doi:10.1139/e80-012 | ||
| In | (1980, January) Canadian Journal of Earth Sciences Vol. 17 (1) Canadian Science Publishing | ||
| Abstract/Notes | U–Pb and Rb–Sr ages performed in the Anti-Atlas (Morocco), especially in Bou Azzer area, demonstrate a Pan-African orogeny (680–570 Ma), along the northern margin of the West African craton (2000 Ma). Geological and geochronological data allow the reconstitution of a coherent succession of events of Pan-African ages. The geodynamic evolution of this domain comprises a stage of oceanic opening (ophiolites) followed with a stage of closure: obduction of the ophiolites on the craton, then subduction under an active continental margin. This segment of the Pan-African belt can be correlated with the other parts of the belt, located on the eastern margin of the West African craton. | ||
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