Hamimi, Z., El-Fakharani, A., Emam, A., Barreiro, J.G., Abdelrahman, E. and Abo-Soliman, M.Y. (2018) Reappraisal of the Kinematic History of Nugrus Shear Zone Using PALSAR and Micro-Structural Data: Implications for the Tectonic Evolution of the Eastern Desert Tectonic Terrane, Northern Nubian Shield. Arabian Journal of Geosciences, 11, Article No. 494.
https://doi.org/10.1007/s12517-018-3837-3

has been cited by the following article:

• TITLE: Lineaments Extraction and Analysis Using Landsat 8 (OLI/TIRS) in the Northeast of Morocco

  AUTHORS: Meryem Redouane, Hicham Si Mhamdi, Faouziya Haissen, Mohammed Raji, Othman Sadki

  KEYWORDS: Northeastern Morocco, Rif Belt, Faults, Miocene-Plio Quaternary Volcanism, Permeability, Lineaments, Landsat 8 (OLI/TIRS)

  JOURNAL NAME: Open Journal of Geology, Vol.12 No.5, May 27, 2022

  ABSTRACT: Northeastern Morocco is made up of several units belonging to the Alpine belt and its foreland. Miocene to plio-quaternary volcanic rocks with variable mineralogy and geochemistry dominate the geology of this region. The presence of active faults in different directions explains the high tectonic instability and the high frequency of earthquakes. This study contributes to the effort of understanding the geothermal potential of the Northeast of Morocco. Heat source and permeability are both key factors in the geothermal process. Indeed, lineaments analysis constrains the structures and their directions and indicates severely faulted zones, which are the most promising areas for geothermal exploration. For this purpose, we used Landsat data combined with geological and structural maps available in this region. Different image processing techniques were applied including band ratio (6/2) and directional filters. To validate the results, we conducted a comparative study between linear structures, available geological data, and previous studies. Results of the automatic extraction method of lineaments from Landsat 8 OLI/TIRS indicate three main lineament systems: 1) a NE-SW system ranging from N40 to N70; 2) an N-S system ranging from N10 to N45; 3) an EW to WNW-ESE systems ranging from N80 to N120. Most of lineaments extracted are localized in Kebdana, Amejjaou, Nador and Melilla regions. Compared to previous studies, the NE-SW system is consistent with an extensive period (Tortonian to Pliocene); the NW-SE system is consistent with the last compressive episode (Pliocene); the N-S system is consistent with the first compressive period (Late/End Tortonian).