Lithological mapping using Landsat 8 Oli multispectral data in Boumalne, Imider, and Sidi Ali Oubork, High Central Atlas, Morocco
The recognition of geological formations, from a lithological point of view, as well as their tectonic character always remain a major challenge for any precise geological study, in this work we will see the great importance of the application of remote sensing (Landsat OLI, DEM) to realize litholog...
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doaj-70d8273af4af4a6c85a8c6ac5787d0492021-02-18T10:35:52ZengEDP SciencesE3S Web of Conferences2267-12422021-01-012340001710.1051/e3sconf/202123400017e3sconf_icies2020_00017Lithological mapping using Landsat 8 Oli multispectral data in Boumalne, Imider, and Sidi Ali Oubork, High Central Atlas, MoroccoAbdelouhed Farah0Algouti Ahmed1Algouti Abdellah2Ait Mlouk Mohamed3Ifkirne Mohammed4Cadi Ayyad University, Faculty of Sciences, Department of GeologyCadi Ayyad University, Faculty of Sciences, Department of GeologyCadi Ayyad University, Faculty of Sciences, Department of GeologyCadi Ayyad University, Faculty of Sciences, Department of GeologyCadi Ayyad University, Faculty of Sciences, Department of GeologyThe recognition of geological formations, from a lithological point of view, as well as their tectonic character always remain a major challenge for any precise geological study, in this work we will see the great importance of the application of remote sensing (Landsat OLI, DEM) to realize lithological maps of great interest as well as the realization of detailed lineament maps with the statistics of the performed measurements, the application of some indicated techniques showed a good discrimination of the lithology of geological formations (Fig.8 ,Fig.10,Fig.11),better results and interpretations are also obtained for lineaments affecting the whole area by using the CP1 and DEM methods (Fig.5,Fig.6).Topographic map and geological maps of JBEL SAGHRO DADES and TODGHA MADER (1/200000) gained from ministry of energy and mines, direction of geology (1975), are used for validation of the obtained results by eliminating of artificial structures (roads) and geological layer boundaries. All data sets were pre-processed and projected in the Universal Transverse Mercator (UTM Zone 29 North) projection system and the WGS84 datum using GIS tools (ArcGIS 10.2).https://www.e3s-conferences.org/articles/e3sconf/pdf/2021/10/e3sconf_icies2020_00017.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Abdelouhed Farah Algouti Ahmed Algouti Abdellah Ait Mlouk Mohamed Ifkirne Mohammed |
spellingShingle |
Abdelouhed Farah Algouti Ahmed Algouti Abdellah Ait Mlouk Mohamed Ifkirne Mohammed Lithological mapping using Landsat 8 Oli multispectral data in Boumalne, Imider, and Sidi Ali Oubork, High Central Atlas, Morocco E3S Web of Conferences |
author_facet |
Abdelouhed Farah Algouti Ahmed Algouti Abdellah Ait Mlouk Mohamed Ifkirne Mohammed |
author_sort |
Abdelouhed Farah |
title |
Lithological mapping using Landsat 8 Oli multispectral data in Boumalne, Imider, and Sidi Ali Oubork, High Central Atlas, Morocco |
title_short |
Lithological mapping using Landsat 8 Oli multispectral data in Boumalne, Imider, and Sidi Ali Oubork, High Central Atlas, Morocco |
title_full |
Lithological mapping using Landsat 8 Oli multispectral data in Boumalne, Imider, and Sidi Ali Oubork, High Central Atlas, Morocco |
title_fullStr |
Lithological mapping using Landsat 8 Oli multispectral data in Boumalne, Imider, and Sidi Ali Oubork, High Central Atlas, Morocco |
title_full_unstemmed |
Lithological mapping using Landsat 8 Oli multispectral data in Boumalne, Imider, and Sidi Ali Oubork, High Central Atlas, Morocco |
title_sort |
lithological mapping using landsat 8 oli multispectral data in boumalne, imider, and sidi ali oubork, high central atlas, morocco |
publisher |
EDP Sciences |
series |
E3S Web of Conferences |
issn |
2267-1242 |
publishDate |
2021-01-01 |
description |
The recognition of geological formations, from a lithological point of view, as well as their tectonic character always remain a major challenge for any precise geological study, in this work we will see the great importance of the application of remote sensing (Landsat OLI, DEM) to realize lithological maps of great interest as well as the realization of detailed lineament maps with the statistics of the performed measurements, the application of some indicated techniques showed a good discrimination of the lithology of geological formations (Fig.8 ,Fig.10,Fig.11),better results and interpretations are also obtained for lineaments affecting the whole area by using the CP1 and DEM methods (Fig.5,Fig.6).Topographic map and geological maps of JBEL SAGHRO DADES and TODGHA MADER (1/200000) gained from ministry of energy and mines, direction of geology (1975), are used for validation of the obtained results by eliminating of artificial structures (roads) and geological layer boundaries. All data sets were pre-processed and projected in the Universal Transverse Mercator (UTM Zone 29 North) projection system and the WGS84 datum using GIS tools (ArcGIS 10.2). |
url |
https://www.e3s-conferences.org/articles/e3sconf/pdf/2021/10/e3sconf_icies2020_00017.pdf |
work_keys_str_mv |
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