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Content available Applying Remotely Sensed Imagery to Extract Geological Lineaments South Rifian Ridges, Morocco
El Aoufir Mohammed, Benabbou Mohamed, Benzougagh Brahim, Sassioui Slimane, El Asmi Hicham, Elkourchia Abdelfattah, Elabouyi Mustapha
Ecological Engineering & Environmental Technology
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2024
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Vol. 25, iss. 7
118--132
EN
The South Rifain ridges are an example of tectonic-sedimentation interaction in the Mio-Plio-Quaternary foreland basins at the front of the Rif chain. is an elongated mountain zone-oriented E-W and N-S, forming the most frontal part of the Rif belt. The morphotectonic study carried out in this area is based on Landsat-8 OLI image processing techniques to determine the contribution of these images to structural mapping. The results obtained reveal a predominant E-W orientation, which is widely present throughout the study area. This is followed by a second N-S direction, a third NW-SE direction, and a fourth NE-SW direction. The NW-SE lineaments are also mapped in kilometres. Their equivalent on the ground shows a sinister movement but does not show a significant horizontal displacement of more than a few metres. Together with the NE-SW faults, these faults form a conjugate system of dextral and sinistral faults, compatible with a palaeostress field where the maximum shortening stress is submeridian.
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