Post-Hercynian ultrahigh-temperature tectono-metamorphic evolution of the Middle Atlas lower crust (central Morocco) revealed by metapelitic granulite xenoliths
- DOI
- 10.5194/se-16-1-2025
- Published
- 01
- Container
- Solid Earth
- Publisher
- Not recorded
- Open access
- yes
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Cite this work
BibTeX
@article{allodium:10.5194/se-16-1-2025,
title = {Post-Hercynian ultrahigh-temperature tectono-metamorphic evolution of the Middle Atlas lower crust (central Morocco) revealed by metapelitic granulite xenoliths},
author = {A. El Maz and A. Vauchez and J.-M. Dautria},
year = {2025},
journal = {Solid Earth},
doi = {10.5194/se-16-1-2025},
url = {https://doi.org/10.5194/se-16-1-2025}
}RIS
TY - JOUR TI - Post-Hercynian ultrahigh-temperature tectono-metamorphic evolution of the Middle Atlas lower crust (central Morocco) revealed by metapelitic granulite xenoliths AU - A. El Maz AU - A. Vauchez AU - J.-M. Dautria PY - 2025 JO - Solid Earth DO - 10.5194/se-16-1-2025 UR - https://doi.org/10.5194/se-16-1-2025 ER -
APA
Maz, A. E., Vauchez, A., & Dautria, J. (2025). Post-Hercynian ultrahigh-temperature tectono-metamorphic evolution of the Middle Atlas lower crust (central Morocco) revealed by metapelitic granulite xenoliths. Solid Earth. https://doi.org/10.5194/se-16-1-2025