The tectonic structures of the Mako area in the Kédougou-Kéniéba inlier (KKI) were mapped with tele-analytical investigation which is validated by field data. This study is based on different images pro...The tectonic structures of the Mako area in the Kédougou-Kéniéba inlier (KKI) were mapped with tele-analytical investigation which is validated by field data. This study is based on different images processing in particular: </span><span style="font-family:Verdana;">1</span><span style="font-family:""><span style="font-family:Verdana;">) the colored combinations (1 to 5) and panchromatic (8) thematic mapping bands of the Landsat-8 (ETM</span><sup><span style="font-family:Verdana;">+</span></sup><span style="font-family:Verdana;">) satellite;</span></span><span style="font-family:Verdana;">2</span><span style="font-family:Verdana;">) Digital Elevation Model (DEM) image of Space Shuttle Radar Topography Mission (SRTM);</span><span style="font-family:Verdana;">3</span><span style="font-family:""><span style="font-family:Verdana;">) airborne geophysics (aeromagnetic and radiometric) images. In these images, four major directions of lineaments NS, NNE-SSW, NW-SE and EW would be related to the tectonic structures, have been identified and mapped. Field data confirm these four structural directions and show that most of these lineaments are related to faults, shear and/or thrust zones, or even basic rock dykes. N-S to NE-SW oriented lineaments are more frequent followed by those NW-SE oriented. These two directions of lineaments are generally in correlation with trajectories of major sinistral shear zones in the Mako area. They would be associated with the S</span><sub><span style="font-family:Verdana;">2a</span></sub><span style="font-family:Verdana;"> and S</span><sub><span style="font-family:Verdana;">2b</span></sub><span style="font-family:Verdana;"> schistosities relative to the D</span><sub><span style="font-family:Verdana;">2</span></sub><span style="font-family:Verdana;"> Eburnean major deformation. They often intersect the E-W oriented lineaments which are less frequent and sometimes folded and crenulated. This E-W oriented linea</span><span><span style="font-family:Verdana;">ment would be prior and are asso展开更多
文摘The tectonic structures of the Mako area in the Kédougou-Kéniéba inlier (KKI) were mapped with tele-analytical investigation which is validated by field data. This study is based on different images processing in particular: </span><span style="font-family:Verdana;">1</span><span style="font-family:""><span style="font-family:Verdana;">) the colored combinations (1 to 5) and panchromatic (8) thematic mapping bands of the Landsat-8 (ETM</span><sup><span style="font-family:Verdana;">+</span></sup><span style="font-family:Verdana;">) satellite;</span></span><span style="font-family:Verdana;">2</span><span style="font-family:Verdana;">) Digital Elevation Model (DEM) image of Space Shuttle Radar Topography Mission (SRTM);</span><span style="font-family:Verdana;">3</span><span style="font-family:""><span style="font-family:Verdana;">) airborne geophysics (aeromagnetic and radiometric) images. In these images, four major directions of lineaments NS, NNE-SSW, NW-SE and EW would be related to the tectonic structures, have been identified and mapped. Field data confirm these four structural directions and show that most of these lineaments are related to faults, shear and/or thrust zones, or even basic rock dykes. N-S to NE-SW oriented lineaments are more frequent followed by those NW-SE oriented. These two directions of lineaments are generally in correlation with trajectories of major sinistral shear zones in the Mako area. They would be associated with the S</span><sub><span style="font-family:Verdana;">2a</span></sub><span style="font-family:Verdana;"> and S</span><sub><span style="font-family:Verdana;">2b</span></sub><span style="font-family:Verdana;"> schistosities relative to the D</span><sub><span style="font-family:Verdana;">2</span></sub><span style="font-family:Verdana;"> Eburnean major deformation. They often intersect the E-W oriented lineaments which are less frequent and sometimes folded and crenulated. This E-W oriented linea</span><span><span style="font-family:Verdana;">ment would be prior and are asso
