Geological Exploration of Marble Deposits in Toto Area, Nasarawa State, Nigeria
- 1 Université Dandicko Dankoulodo de Maradi, Maradi, Niger
- 2 Nasarawa State University, Keffi, Nigeria
- 3 School of Geography, Earth and Environmental Sciences, University of Plymouth, Plymouth, UK
Abstract
Geological mapping as well as chemical analysis for marble deposit in the Muro-Obugu-Panda area of Toto Local Government, Nasarawa State, Nigeria, was carried out. The objectives of the study are to first map out the extent of the deposit and then evaluate its chemical characteristics. The geology of the area forms part of the Upper Proterozoic low-grade (green schist facies) schist belts of Central Nigeria, and consists of schists, banded iron, quartzite, and marble. Geological mapping revealed that the marble deposit stretches in a NE-SW direction, from Muro in the north to Kolo in the south, covering about 28 km2. This deposit consists mainly of silicified gray and white varieties of marble. The mapping also identified three (3) exploration targets A—Panda, B—Obugu, and C— Soka. Chemical analysis of eight (8) selected samples shows that CaO content varies from 3.72 to 53.12 wt%. Other impurities are Fe 2 O 3 , Al 2 O 3 , MgO and SiO 2 . Plot of Na 2 O + K 2 O vs. SiO 2 shows a positive correlation while that of CaO and MgO exhibits a well defined negative correlation with SiO2 and this reflects the introduction of chert during the deposition of the parent limestone of the marble body. The variation plot of CaO vs. MgO shows an inverse relationship. This is reflected in the inverse relationship in the proportion of calcite to dolomite in the marble. All these results correlate with those found in the adjacent area by previous workers and this indicates the same extension of marble in these areas. The Muro marble can be used economically as raw materials for a variety of products such as fillers, glass, papers, lime, pesticide and sewage treatment, decorative construction, monuments, paint making and most of all very suitable for cement production.
- Ajibade, A.C. (1976) Provisional Classification and Correlation of Schists Belts in Northwestern Nigeria. In: Kogbe, C.A., Ed., Geology of Nigeria, Elizabethan Pub. Co., Lagos, 88-90.
- Grant, N.K. (1970) Geochronology of Precambrian Basement Rocks from Ibadan, South-Western Nigeria. Earth and Planetary Sciences Letter, 10, 19-38. http://dx.doi.org/10.1016/0012-821X(70)90061-0
- Turner, D.C. (1983) Upper Proterozoic Schist Belt in the Nigerian Sector of Pan African Province of West Africa. In: Kogbe, C.A., Ed., Geology of Nigeria, 2nd Revised Edition, Rock-view Limited, Jos, Nigeria.
- Ajibade, A.C., Fitches, W.R. and Wright, J.B. (1979) The Zungeru Mylonites, Nigeria: Recognition of a Major Unit. Revue de Géologie et Géographie Physique, 21, 359-363.
- Jones, H.A. and Hockney, R.D. (1964) The Geology of Parts of Southwestern Nigeria. Bulletin, Geological Survey of Nigeria, 31, 101.
- Rahman, M.A. (1992) Precambrian Geology of Nigeria. Proceedings of High Grade Terrains Benin-Nigeria Traverse, Programme and Lecture Series, 150-200.
- Odeyemi, I.B (1988) Lithostratigraphic and Structural Relationships of the Upper Precambrian Metasediments in Igarra Area, Western Nigeria. The Precambrian Geology of Nigeria, Geological Survey of Kaduna, 111-123.
- Ekweme, B.N. (1990) Petrology of Southern Obodu Plateau Bamenda Massif, Southeastern Nigeria. In: Rocci, G. and Deschamps, M.., Eds., Recent Data in African Earth Sciences, CIFEG Occasional Publication, 22, 155-158.
- Ekweme, B.N. (2000) Zircon Evaporation Ages from Obudu Plateau First Evidence of Archean Components in the Schist of Southeastern, Nigeria. 37th Nigerian Mining and Geosciences Conference, Jos, Book of Abstracts.
- Talal, M.Q. (2000) Testing Jabal Farasan Marble Deposit for Multiple Industrial Applications. Arabian Journal for Science and Engineering, 33, 79-97.
- Lipmann, F. (1973) Sedimentary Carbonate Minerals. Springer Verlag, Berlin Heidelberg, New York, 229 p. http://dx.doi.org/10.1007/978-3-642-65474-9
- Obasi, R.A. (2012) Geochemical and Appraisal of the Economic Potential of Calc-Gneiss and Marble from Igaara, Edo State, Southwest, Nigeria. Journal of Science and Technology, 2, 1018-1021.
- Goldschmidth, J.R., Graff, L. and Joensu, O.I. (1955) The Occurrence of Magnesium Calcite in Nature. Geochimica et Cosmochimica Acta, 1, 212-230. http://dx.doi.org/10.1016/0016-7037(55)90033-8