Integration of remote sensing and geophysical methods for structural and lithological mapping in a part of Precambrian Basement Rocks, northern Nigeria

Landsat 8 OLI data, Aeromagnetic and Radial Vertical Electrical Sounding (RVES) survey data were integrated to map lithology, delineate structures their trends, possible mineralized zones in the area. yielded a color composite image, surface lineaments of The aeromagnetic maps utilized subsurface structures. A radial confirmed fractures derived from structural maps. Results classified area into three geological units viz: migmatite, banded gneiss, quartzite. gneiss is most deformed contains series that are significant for mineral groundwater explorations. Clay alteration dominant area, followed by iron oxide alterations. Lineament alignments N-S, NNW-SSE, NNE-SSW, NE-SW, E-W directions.