Reconstruction and appraisal of Akunu–Akoko area iron ore deposits using geological and magnetic approaches

Geological mapping and magnetic methods were applied for the exploration of iron ore deposits in the Akunu–Akoko area of Southwestern Nigeria for the purpose of evaluating their geological characteristics and resource potentials. A proton magnetometer measures the vertical, horizontal and total magn...

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Main Authors: Okpoli Cyril, Akingboye Adedibu
Format: Article
Language:English
Published: Sciendo 2016-06-01
Series:Materials and Geoenvironment
Subjects:
Online Access:https://doi.org/10.1515/rmzmag-2016-0003
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spelling doaj-f4b9bcb32f464f8185e3d46d2c6ac3812021-09-05T14:00:20ZengSciendoMaterials and Geoenvironment1854-74002016-06-01631193810.1515/rmzmag-2016-0003rmzmag-2016-0003Reconstruction and appraisal of Akunu–Akoko area iron ore deposits using geological and magnetic approachesOkpoli Cyril0Akingboye Adedibu1Department of Earth Sciences, Adekunle Ajasin University, Akungba–Akoko, Ondo State, NigeriaDepartment of Earth Sciences, Adekunle Ajasin University, Akungba–Akoko, Ondo State, NigeriaGeological mapping and magnetic methods were applied for the exploration of iron ore deposits in the Akunu–Akoko area of Southwestern Nigeria for the purpose of evaluating their geological characteristics and resource potentials. A proton magnetometer measures the vertical, horizontal and total magnetic intensities in gammas. The subsurface geology was interpreted qualitatively and quantitatively. The downward continuations and second vertical derivatives, the small-sized mineralised bodies and shallow features in the study area were mapped. The faults are trending in the following directions: NE–SW, NW–SE, N–S and E–W groups, while the iron ore mineralisation is structurally controlled by two major groups of fault trends, namely, the NE–SW and NW–SE; the N–S and E–W groups are mere occurrences that do not contribute to the structural control of the iron ore mineralisation in Akunu.https://doi.org/10.1515/rmzmag-2016-0003magnetic methodgeological mappingquantitative interpretationakununigeria
collection DOAJ
language English
format Article
sources DOAJ
author Okpoli Cyril
Akingboye Adedibu
spellingShingle Okpoli Cyril
Akingboye Adedibu
Reconstruction and appraisal of Akunu–Akoko area iron ore deposits using geological and magnetic approaches
Materials and Geoenvironment
magnetic method
geological mapping
quantitative interpretation
akunu
nigeria
author_facet Okpoli Cyril
Akingboye Adedibu
author_sort Okpoli Cyril
title Reconstruction and appraisal of Akunu–Akoko area iron ore deposits using geological and magnetic approaches
title_short Reconstruction and appraisal of Akunu–Akoko area iron ore deposits using geological and magnetic approaches
title_full Reconstruction and appraisal of Akunu–Akoko area iron ore deposits using geological and magnetic approaches
title_fullStr Reconstruction and appraisal of Akunu–Akoko area iron ore deposits using geological and magnetic approaches
title_full_unstemmed Reconstruction and appraisal of Akunu–Akoko area iron ore deposits using geological and magnetic approaches
title_sort reconstruction and appraisal of akunu–akoko area iron ore deposits using geological and magnetic approaches
publisher Sciendo
series Materials and Geoenvironment
issn 1854-7400
publishDate 2016-06-01
description Geological mapping and magnetic methods were applied for the exploration of iron ore deposits in the Akunu–Akoko area of Southwestern Nigeria for the purpose of evaluating their geological characteristics and resource potentials. A proton magnetometer measures the vertical, horizontal and total magnetic intensities in gammas. The subsurface geology was interpreted qualitatively and quantitatively. The downward continuations and second vertical derivatives, the small-sized mineralised bodies and shallow features in the study area were mapped. The faults are trending in the following directions: NE–SW, NW–SE, N–S and E–W groups, while the iron ore mineralisation is structurally controlled by two major groups of fault trends, namely, the NE–SW and NW–SE; the N–S and E–W groups are mere occurrences that do not contribute to the structural control of the iron ore mineralisation in Akunu.
topic magnetic method
geological mapping
quantitative interpretation
akunu
nigeria
url https://doi.org/10.1515/rmzmag-2016-0003
work_keys_str_mv AT okpolicyril reconstructionandappraisalofakunuakokoareaironoredepositsusinggeologicalandmagneticapproaches
AT akingboyeadedibu reconstructionandappraisalofakunuakokoareaironoredepositsusinggeologicalandmagneticapproaches
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