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Interprétation géodynamique du domaine pan-africain (Précambrien terminal) de l'Anti-Atlas (Maroc) à partir de données géologiques et géochronologiques

Leblanc, M., Lancelot, J. R.·1980·Canadian Journal of Earth Sciences

Abstract

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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Metadata

Authors
Leblanc, M., & Lancelot, J. R.
Venue
Canadian Journal of Earth Sciences
Published
1980-01-01
Volume
17
Issue
1
Pages
142-155
ISSN
  • 0008-4077 (ISSN-L)
  • 1480-3313
OpenAlex
W2012609187
Cited by
195
References
0
FWCI
3.45
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Interprétation géodynamique du domaine pan-africain (Précambrien terminal) de l'Anti-Atlas (Maroc) à partir de données géologiques et géochronologiques. https://app.cochat.ai/papers/10.1139/e80-012
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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. https://doi.org/10.1139/e80-012

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