ANALYSIS OF LINEAMENT MAP OF PART OF MARU SCHIST BELT, NORTHWEST, NIGERIA AND ITS IMPLICATION FOR MINERAL EXPLORATION

  • Joe O. Osumeje Dept. of Physics, A.B.U., Zaria
  • A. S. Oniku
  • O. C. Meludu
Keywords: Aeromagnetic, Lineaments, Mineral, Remote sensing, and Schist-Belt

Abstract

Lineament are extended mappable linear or curvilinear feature of a surface which can be utilized in mineral, oil, gas, and underground water studies. They are obvious in satellite images, aerial images or aerial photographs. The aim of this study is to analyse an automatically generated lineament from part of the Maru schist belt using a combination of Digital Elevation Model (DEM) data and Aeromagnetic data. The area of study is within the Maru schist belt in Zamfara State. A shaded relief map was produced from the two data sources and the lineament was extracted automatically from them. The extracted lineament was combined to obtain a final lineament map of the area. Trends such as N-S, NW–SE, ENE–WSW and NW–SE, with very little E-W were all present. The areas of very high, high, moderate and low population of lineaments was delineated. Regions with very high lineament intersections and lineament concentration, covers an area of 153.6 km2 and accounts for 16.1% of the study area, these regions are known to harbour gold and iron ores from literature reviews. These target regions are located at the Northern and South part of the study area. Also, the gold artisan miners have dominated these same regions and they have only started from exposed vein of gold mineralization. With this rather fast and easier approach of obtaining such a map, it could be used as a start point for planning a more detailed geophysical or geological survey

References

Adekoya, J. A. (1996). The Nigerian schist belt: Age and Depositional environment implications from associated banded iron –formations. Journal Mining and Geology, 32:27-46.

Alizadeh, H. and Arian, M. (2015) Rule of Structural Factors in Formation of Porphyry Copper

Deposits in South Western Part of Kerman Area, Iran. Open Journal of Geology, 5:489-498. doi: 10.4236/ojg.2015.57045.

Chernicoff, C. J., Richards, J. P. and Zappettini, E. O. (2002). Crustal lineament control on

magmatism and mineralization in Northwestern Argentina: geological, geophysical, and remote sensing evidence. Ore Geology Reviews, 21:127–155.

Danbatta, U.A. (2003). The tecteonic significance of the NNE- continuation of the Kalangai fault zone into Kazaure Schist Belt of NW Nigeria. Science Africana, 2(1 and 2): 17-25.

Hardcastle, K. C., (1995). Photo-lineament factor: a new computer-aided method for remotely

sensing the degree to which bedrock is fractured, Photogrammetric Engineering & Remote Sensing, 61(6):739-747

Haruna, I.V., (2017). Review of the Basement Geology and Mineral Belts of Nigeria, Journal of

Applied Geology and Geophysics, 5(1):37-45.

Ibrahim, A. A. (2012). Formation of Atoll Garnets in the Banded Iron Formation of Maru

Schist Belt. American International Journal of Contemporary Research, 2(5).

Kolawole, F. and Anifowose, A. Y. B. (2011). Remote sensing analysis of a dextral discontinuity along Ifewara-Zungeru area, Nigeria, West Africa. Indian Journal of Science and Technology 4(1): 46-51.

Kudamnya, E.A., Andongma, W.T. and Osumeje, J.O., (2014). Hydrothermal mapping using remote sensing technique of the Maru schist belt. International Journal of Civil Engineering (IJCE),1(3):59-66.

Masoud, A. and Koike, K. (2011). Morphotectonics Inferred from the Analysis of Topographic Lineaments Auto-Detected from DEMs: Application and Validation for the Sinai Peninsula, Egypt. Tectonophysics, 510(1-2): 291-308.

Obaje, N. G. (2009). Geology and Mineral Resources of Nigeria. Lecture Notes in Earth Sciences. Volume 120. Springer-Verlag Berlin Heidelberg.

Oke, S. A., Abimbola, A. F., and Rammlmair, D., (2014). Mineralogical and Geochemical Characterization of Gold Bearing Quartz Veins and Soils in Parts of Maru Schist Belt Area, Northwestern Nigeria, Journal of Geological Research, Volume 2014, Article ID 314214.

Prabu, P., & Rajagopal, B. (2013). Mapping of Lineaments for Groundwater Targeting and Sustainable Water Resource Management in Hard Rock Hydrogeological Environment Using RS- GIS. Climate Change and Regional/Local Responses. doi:10.5772/55702.

Rowan, L.C. and Wetlaufer, P.H. (1975). Iron absorption band analysis for the discrimination of iron rich zones: U.S. Geological Survey, Type III Final Report, Contract S-70243-AG, pp.125.

Sanusi, S. O. and Amigun, J. O. (2020). Structural and hydrothermal alteration mapping related to orogenic gold mineralization in part of Kushaka schist belt, North central Nigeria, using airborne magnetic and gamma ray spectrometry data. SN Applied Sciences, Springer Nature Switzerland, 2:1591

Seleem, T. A. (2013). Analysis and Tectonic Implication of DEM-Derived Structural Lineaments, Sinai Peninsula, Egypt. International Journal of Geosciences, 4: 183-201.

Solomon S. and Ghebreab, G. (2006). Lineament Characterization and Their Tectonic Significance Using Landsat TM Data and Field Studies in the Central Highlands of Eritrea. Journal of African Earth Sciences, 46(4): 371-378.

Published
2021-11-04
How to Cite
OsumejeJ. O., OnikuA. S., & MeluduO. C. (2021). ANALYSIS OF LINEAMENT MAP OF PART OF MARU SCHIST BELT, NORTHWEST, NIGERIA AND ITS IMPLICATION FOR MINERAL EXPLORATION. FUDMA JOURNAL OF SCIENCES, 5(3), 355 - 362. https://doi.org/10.33003/fjs-2021-0503-721