- 1Mohammadia School of Engineers (EMI), Mohammed V University (UM5), Rabat, Morocco
- 2National Office of Hydrocarbons and Mines (ONHYM), Rabat, Morocco
- 3Faculty of Science and Technology (FST), Cadi Ayyad University (UCA), Marrakesh, Morocco
- 4Geosciences Montpellier (UM), University of Montpellier, CNRS, Montpellier, France
The Anti-Atlas, one of the oldest mountain chains in Morocco, has undergone multiple orogenic events that shaped its complex geology, making it a major province of sediment-hosted copper deposits, particularly in its western part. This study adopts a multi-scale, interdisciplinary workflow combining high-resolution hyperspectral remote sensing (up to 5 m spatial resolution), field-based spectral validation, geochemical analyses, and airborne geophysical data to achieve a comprehensive characterization of mineralization processes. Regional mapping of structural lineaments and copper-related alteration zones guided field investigations and the sampling of both mineralized and non-mineralized facies, allowing constraints to be placed on the origin of mineralization. These surface observations were subsequently linked to subsurface architecture through airborne geophysical modelling of regional geological cross-sections derived from field data. The integrated interpretation of all datasets enabled the development of a coherent geodynamic model adapted to the Alma Inlier. Overall, the proposed approach enhances exploration efficiency, reduces uncertainty, and supports more sustainable mineral exploration strategies.
Keywords: Western Anti-Atlas, copper deposits, Hyperspectral remote sensing, Geochemical and geophysical integration, Exploration
How to cite: M'hamdi Alaoui, I., Akhssas, A., Bahi, A., Gautier, S., Ibouh, H., Berkat, N. E., Boumehdi, M., Khebbi, H., and Abouabila, Y.: From Space to Field: Multi-Scale Characterization of Sediment-Hosted Copper Deposits in the Alma Inlier, Western Anti-Atlas, Morocco, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-20552, https://doi.org/10.5194/egusphere-egu26-20552, 2026.