International Peer-Reviewed JournalOpen AccessISSN 2456-8880
irejournals@gmail.com+91-7433024337

Home / Current Issue / Paper 1702691

1702691 Vol 4 · Issue 11 Download Paper

Geophysical Characterization of Candidate Rock Contacts Within Igarra Area, South-western Nigeria

MUSLIM B. AMINU

Subject area: Science,Engineering and Technology  ·  Area of research: Earth Science

Abstract

The aim of this paper is to present the application and interpretation of multi-method nearsurface geophysical surveys including electrical resistivity imaging, total-field ground magnetic prospecting and ground electrical conductivity surveying to delineate lateral rock contacts in Igarra area in Southwestern Nigeria, especially in locations of poor rock exposure. The multi-method technique has practical application in detecting fracture zones for groundwater resource development; besides, the usefulness in improving the placement of locations of rock contacts accurately on geological maps. In the Igarra area, the lateral lithologic contacts have resulted from the metamorphism and re-crystallisation of initial contacts between sedimentary rocks, and also from late-stage granitic intrusions into pre-existing meta-sediments. Three geophysical profiles were taken in the study area. The profiles traverse contacts involving a transition from metaconglomerate-to-intrusive granite and two re-crystallized and rotated sedimentary boundaries; a metaconglomerate-to-quartzite and a phyllite-to-metaconglomerate boundary. Each boundary type yielded consistent diagnostic ground electrical resistivity and total field magnetic anomalies indicative of either the presence of groundwater or magnetic mineral concentrations at the contacts. The metaconglomerate-to-quartzite contact presented an electrical conductivity anomaly. However, the metaconglomerate-to-intrusive granite and the phyllite-to-metaconglomerate boundary did not present any electrical conductivity anomaly. The delineated rock contacts are potential supplementary source of groundwater and possible locations for the concentration of valuable minerals in the Igarra area.

Keywords

Lithologic contacts, near surface geophysics, low aperture fractures, groundwater, Igarra Schist belt

References

[1] Aminu, M. B., Akande, T. M. and Ishola, A. O. -2D Geoelectric Imaging of the Uneme-Nekhua Fracture Zone. International Journal of Geophysics, 2014. http://dx.doi.org/10.1155/2014/842812

[2] Aminu, M. B. -Electrical Resistivity Imaging of a Thin Clayey Aquitard Developed on Basement Rocks in Parts of Adekunle Ajasin University Campus, Akungba-Akoko, South-western Nigeria. Environmental Research, Engineering and Management, vol. 71, no. 1, pp. 47-55. 2015a.

[3] Aminu, M. B. -Geo-electric Investigation of the Cause of Structural Failure Indices on a Set of Administrative Blocks. Journal of Applied Geology and Geophysics, vol. 3, no. 4, pp. 1-10, 2015b.

[4] Aminu, M. B. -Subsurface Electrical Resistivity Imaging and Electromagnetic Conductivity Profiling at a Proposed Construction Site at Adekunle Ajasin University Campus, Akungba-Akoko, South-Western Nigeria. Global Journal of Geological Sciences, vol. 16, pp. 53-60, 2018.

[5] Annor A.E. -Structural and Chronological relationship between the low grade Igarra Schist and adjoining Okene Migmatite-Gneiss terrain in the Precambrian exposure of Southwestern Nigeria. Journal of Mining and Geology, vol. 34, pp. 194-97, 1998.

[6] Anderson, N. L. -Selection of Appropriate Geophysical Techniques: A Generalized Protocol Based on Engineering Objectives and Site Characteristics. Proc., 2006 Highway NDE Conference, 2006, pp. 29-47. http://2006geophysics.mst.edu/.

[7] Booth, A. D., Vandeginste, V., Pike, D., Abbey, R., Clark, R. A., Green, C. M. and Howland, N. -Geochemical constraints in near-surface geophysical surveying from in situ XRF spectrometry: Field trials at two aviation archaeology sites. In: Persico, R., Piro, S. and Linford, N. (Eds). Innovation in Near-Surface Geophysics: Instrumentation, Application, and Data Processing Methods. Elsevier, 2019, pp. 97-119.

[8] Bufford, K. M., Atekwana, E. A. and Abdelsalam, M. G. -Geometry and faults tectonic activity of the Okavango Rift Zone, Botswana: evidence from magnetotelluric and electrical resistivity tomography imaging. Journal of African Earth Sciences, vol. 65, pp. 61-71, 2012.

[9] Chavez, R. E., Cifuentes-Nava, G., Tejero, A., Hernandez-Quintero, J. E., and Vargas, D. -Special 3D electric resistivity tomography (ERT) array applied to detect buried fractures on urban areas: San Antonio Tecomitl, Milpa Alta, Mexico. Geofisica Internacional vol. 53, no. 4, pp. 425-434, 2014.

[10] Cosenza, P., Marmet, E., Rejiba, F., Cui, Y. J., Tabbagh, A., and Charlery, Y. -Correlations between geotechnical and electrical data: A case study at Garchy in France, Journal of Applied Geophysics, vol. 60, no. 3, pp. 165-178, 2006.

[11] El-Qady, G., Hafez, M., Abdalla, M. A. and Ushijima, K. -Imaging subsurface cavities using geoelectric tomography and ground penetrating radar, Journal of Cave and Karst Studies, vol, 67, no. 3, pp. 174-181, 2005.

[12] Ekwe, A., Opara, A. and Onwuka, O. -Geoelectrical study of corrosivity and competence of soils within Uburu and Okposi areas of Ebonyi State, Southeastern Nigeria. Anti-Corrosion Methods and Materials, vol. 65, no. 6, pp. 637-645, 2018.

[13] Frid, V., Liskevich, G., Doudkinski, D. and Korostishevsky, N. -Evaluation of landfill disposal boundary by means of electrical resistivity imaging. Environmental Geology, vol. 53, no. 7, pp. 1503-1508, 2008.

[14] Hoover, D.B., Heran, W.D., and Hill, P.L., eds., The geophysical expression of selected mineral deposit models: U.S. Geological Survey Open-file Report 92-557, 1992, 129 p.

[15] Kataka, M. O., Mundalamo R. H., Ratshiedena P. E. and Nemasea, T. -Application of geophysical techniques in mineral exploration for potential sulphide deposits in Musina area 5th International Conference on Geological and Environmental Sustainability, August 13-14, 2018, Bali, Indonesia. DOI: 10.4172/2381-8719-C1-017

[16] LaBrecque, D. J., Ramirez, A. L., Daily, W, D., Binley, A. M. and Schima, S. A. -ERT monitoring of environmental remediation processes,” Measurement Science and Technology, vol. 7, no. 3, pp. 375-383, 1996.

[17] Lines, J. P., Bernardes, S., He, J., Zhang, S., Bacchus, S. T., Madden, M., and Jordan, T. -Preferential Groundwater Flow Pathways and Hydroperiod Alterations Indicated by Georectified Lineaments and Sinkholes at Proposed Karst Nuclear Power Plant and Mine Sites. Journal of Sustainable Development, vol. 5, no. 12, pp. 78-116, 2012.

[18] Mohamed, N. E., Brasse, H., Abdelgalil1, M. Y. And Kheiralla, K. M. -Geoelectric and VLF electromagnetic survey on complex aquifer structures, Central Sudan. Comunicacoes Geologicas vol. 99, no. 2, pp. 95-100, 2012.

[19] Odeyemi I. B. -Lithostratigrahic and structural relationship of the upper Precambrian metasediments of the Igarra area, Southwestern Nigeria. In: Oluyide, P.O., Mbonu, W.C., Ogezi, A.E., Egbunike, I.G., Ajibade, A.C., Ana-Umeji, A.C. (Eds.) Precambrian geology of Nigeria. Geological Survey Nigeria Publication, Kaduna, 1988, pp. 111-123.

[20] Ogbe, O. B., Olobaniyi, S.B., Ejeh, O. I., Omo-Irabor, O. O., Osokpor, J., Ocheli, A., Overare, B. -Petrological and structural investigation of rocks around Igarra, Southwestern Nigeria. Ife Journal of Sciences, vol. 20, no. 3, pp. 663-677, 2018.

[21] Park, S. K. and Roberts, J. J. -Conductivity structure of the San Andreas fault, Parkfield, revisited. Geophysical Research Letters, vol. 30, no. 16, pp. 1842, 2003. doi:10.1029/2003GL017689, 2003.

[22] Pazzi, V., Morelli, S. and Fanti, R. -A Review of the Advantages and Limitations of Geophysical Investigations in Landslide Studies. International Journal of Geophysics. 2019. doi.org/10.1155/2019/2983087

[23] Pirajno, F. -Hydrothermal Processes and Wall Rock Alteration. In: Hydrothermal Processes and Mineral Systems. Springer, Dordrecht, 2009, pp. 73-164.

[24] Rahaman, M. A. -Review of the Basement Geology of South-Western Nigeria. In: C. A. Kogbe (Ed), Geology of Nigeria, Nigeria: Rock View Limited), 1989, pp. 39-56.

[25] Rizzo, E., Colella, A., Lapenna, V. and Piscitelli, S. -Highresolution images of the fault-controlled High Agri Valley basin (Southern Italy) with deep and shallow electrical resistivity tomographies. Physics and Chemistry of the Earth, vol. 29, no. 4, pp. 321-327, 2004.

[26] Robineau, B., Join, J. L., Beauvais, A., Parisot, J-C. and Savin, C. -Geoelectrical imaging of a thick regolith developed on ultramafic rocks: groundwater influence,” Australian Journal of Earth Sciences, vol. 54, no. 5, pp. 773-781, 2007

[27] Soupios, P. M., Georgakopoulos. P., Papadopoulos, N., Saltas, V., Andreadakis, A., Vallianatos, F., Sarris, A., and Makris, J. P. -Use of engineering geophysics to investigate a site for a building foundation, Journal of Geophysics and Engineering, vol. 4, no. 1, pp. 94-103, 2007.

[28] Tanner P.W. G. -The flexural-slip mechanism. Journal of Structural Geology. Vol. 11, no 6, pp. 635-655, 1989. ISSN 0191-8141.

[29] Turner, D. C. -Upper Proterozoic Schist Belts in the Nigerian Sector of the Pan-African Province of West Africa. In: C. A. Kogbe (Ed), Geology of Nigeria, Nigeria: Rock View Limited), 1989, pp. 93-109.

[30] Unsworth, M. J., Malin, P. E., Egbert, G. D. and Booker, J. R. -Internal structure of the San Andreas fault at Parkfield, California, Geology, vol. 25, pp. 359-362. 1997

[31] Yassin, R. R., Muhammad, R. F., Taib, S. H., and Al- Kouri, O., (). Application of ERT and Aerial Photographs Techniques to Identify the Consequences of Sinkholes Hazards in Constructing Housing Complexes Sites over Karstic Carbonate Bedrock in Perak, Peninsular Malaysia. Journal of Geography and Geology, vol. 6, no. 3, pp. 55-89. 2014.

[32] Yi, M. J., and Kim, J. H. -Enhancing the resolving power of the least squares inversion with Active Constraint Balancing: SEG Expanded Abstracts, 68 Annual Meeting, New Orleans, 1998, pp. 485-488.

[33] Zume, J. T., Tarhule, A. and Christenson, S. -Subsurface imaging of an abandoned solid waste landfill site in Norman, Oklahoma. Groundwater Monitoring and Remediation, vol. 26, no. 2, pp. 62-69, 2006.

How to cite this paper

MUSLIM B. AMINU "Geophysical Characterization of Candidate Rock Contacts Within Igarra Area, South-western Nigeria" Iconic Research And Engineering Journals Volume 4 Issue 11 2021 Page 144-153
MUSLIM B. AMINU "Geophysical Characterization of Candidate Rock Contacts Within Igarra Area, South-western Nigeria" Iconic Research And Engineering Journals, vol. 4, no. 11, May. 2021
MUSLIM B. AMINU (2021). Geophysical Characterization of Candidate Rock Contacts Within Igarra Area, South-western Nigeria. Iconic Research And Engineering Journals, 4(11).
MUSLIM B. AMINU "Geophysical Characterization of Candidate Rock Contacts Within Igarra Area, South-western Nigeria" Iconic Research And Engineering Journals, vol. 4, no. 11, May. 2021.
@article{1702691,
      author = {MUSLIM B. AMINU},
      title = {Geophysical Characterization of Candidate Rock Contacts Within Igarra Area, South-western Nigeria},
      journal = {Iconic Research And Engineering Journals},
      year = {2021},
      volume = {4},
      number = {11},
      pages = {144-153},
      issn = {2456-8880},
      url = {https://www.irejournals.com/formatedpaper/1702691.pdf},
      abstract = {The aim of this paper is to present the application and interpretation of multi-method nearsurface geophysical surveys including electrical resistivity imaging, total-field ground magnetic prospecting and ground electrical conductivity surveying to delineate lateral rock contacts in Igarra area in Southwestern Nigeria, especially in locations of poor rock exposure. The multi-method technique has practical application in detecting fracture zones for groundwater resource development; besides, the usefulness in improving the placement of locations of rock contacts accurately on geological maps. In the Igarra area, the lateral lithologic contacts have resulted from the metamorphism and re-crystallisation of initial contacts between sedimentary rocks, and also from late-stage granitic intrusions into pre-existing meta-sediments. Three geophysical profiles were taken in the study area. The profiles traverse contacts involving a transition from metaconglomerate-to-intrusive granite and two re-crystallized and rotated sedimentary boundaries; a metaconglomerate-to-quartzite and a phyllite-to-metaconglomerate boundary. Each boundary type yielded consistent diagnostic ground electrical resistivity and total field magnetic anomalies indicative of either the presence of groundwater or magnetic mineral concentrations at the contacts. The metaconglomerate-to-quartzite contact presented an electrical conductivity anomaly. However, the metaconglomerate-to-intrusive granite and the phyllite-to-metaconglomerate boundary did not present any electrical conductivity anomaly. The delineated rock contacts are potential supplementary source of groundwater and possible locations for the concentration of valuable minerals in the Igarra area.},
      keywords = {Lithologic contacts, near surface geophysics, low aperture fractures, groundwater, Igarra Schist belt},
      month = {May},
  }