Authors :
Y.I. Bawa; A.J. Zainab; I.H. Abusufyan
Volume/Issue :
Volume 9 - 2024, Issue 7 - July
Google Scholar :
https://tinyurl.com/4hmr3bb9
Scribd :
https://tinyurl.com/ys3z5cft
DOI :
https://doi.org/10.38124/ijisrt/IJISRT24JUL341
Abstract :
The study area spans from 4°30' E to 5°00' E
in longitude and from 11°00' N to 11°30' N in latitude. A
total of four profiles 400m long were surveyed using
Wenner array configuration with minimal electrode
spacing of 3m and repeated with integer multiple of 3
that explored up to 18m during which apparent
resistivity values were found. Electrical resistivity
tomography has emerged as a powerful geophysical
technique for investigating subsurface structures,
particularly in mineral exploration. This research
explores the application of resistivity tomography in
delineating basement structures associated with
mineralization. Two-dimensional models were analyzed
with the RES2DINV inversion software to achieve
precise interpretations. The results revealed a range of
geological features and variations at different depths.
High resistivity zones indicated the presence of schist
and moderately weathered gneiss with quartz veins,
which are structurally controlled and oriented North-
West and Northeast-Southwest. This technique proved
effective in identifying potential mineral deposits, aiming
to provide a comprehensive overview of the study area
and improve mineral exploration strategies through
resistivity tomography.
Keywords :
Resistivity Tomography, Basement Structure, Mineralization, Mineral Exploration.
References :
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The study area spans from 4°30' E to 5°00' E
in longitude and from 11°00' N to 11°30' N in latitude. A
total of four profiles 400m long were surveyed using
Wenner array configuration with minimal electrode
spacing of 3m and repeated with integer multiple of 3
that explored up to 18m during which apparent
resistivity values were found. Electrical resistivity
tomography has emerged as a powerful geophysical
technique for investigating subsurface structures,
particularly in mineral exploration. This research
explores the application of resistivity tomography in
delineating basement structures associated with
mineralization. Two-dimensional models were analyzed
with the RES2DINV inversion software to achieve
precise interpretations. The results revealed a range of
geological features and variations at different depths.
High resistivity zones indicated the presence of schist
and moderately weathered gneiss with quartz veins,
which are structurally controlled and oriented North-
West and Northeast-Southwest. This technique proved
effective in identifying potential mineral deposits, aiming
to provide a comprehensive overview of the study area
and improve mineral exploration strategies through
resistivity tomography.
Keywords :
Resistivity Tomography, Basement Structure, Mineralization, Mineral Exploration.