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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Main Authors: Abdelouhed Farah, Algouti Ahmed, Algouti Abdellah, Ait Mlouk Mohamed, Ifkirne Mohammed
Format: Article
Language:English
Published: EDP Sciences 2021-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2021/10/e3sconf_icies2020_00017.pdf
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spelling 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
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