Browsing by Author "Onoduku, U. S."

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    Characterization of Pegmatites in Ogodo-Odobola Area of Idah Sheet 267NW, Central Nigeria
    (INTERNATIONAL JOURNAL OF SCIENCE FOR GLOBAL SUSTAINABILITY, 2023-07) Omanayin, Y. A.; Waziri, N. M.; Onoduku, U. S.; Alabi, A. A.
    The pegmatites of Ogodo-Odobola area around Ajaokuta, Central Nigeria belong to the pegmatite belt of Central Nigeria. A detailed geological mapping of the pegmatites and host rocks was conducted with the aim of understanding their mode of occurrence and field relationship and to assess their mineralization potentials. Twelve (12) representative samples of rocks were selected for petrographic analysis. The results show that the area is underlain by migmatite-gneiss, schist, with intrusions of granite and pegmatite. The pegmatites occur in tabular form with varying widths (2 centimetres – 6 metres) and lengths (12 – 200 metres). Principal joint direction is NNE-SSW which is believed to have influenced the pegmatite emplacement. Petrography of the representative rock samples revealed an average mineralogical composition of biotite (23.90%), microcline (22.15%), hornblende (15.05%), quartz (10.65%), plagioclase (10.35%), muscovite (8.00%), myrmekite (0.20%), and opaque and accessory minerals (9.70%). The pegmatites were found to be dominated by microcline and plagioclase feldspars, and then muscovite, biotite, and accessory and opaque minerals. The pegmatite of the Ogodo-Odobola area is worth probing as the results have shown prospect for possible economic minerals. Keywords: Mineralization, Basement Complex, Structural Features, Petrography, Ajaokuta
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    COMPOSITIONAL FEATURES AND Ta-Sn-Nb RARE METAL MINERALIZATION POTENTIAL OF OGODO-ODOBOLA PEGMATITE, CENTRAL NIGERIA
    (Nigerian Mining and Geosciences Society (NMGS), 59th Annual International Conference & Exhibition Book of Abstract, 2024-03) Omanayin, Y. A.; Waziri, N. M.; Onoduku, U. S.; Alabi, A. A.
    Large pegmatite bodies are abundant in Ogodo-Odobola area. They occur in tabular forms and concordant to discordantly intruding the host rocks of migmatitic gneiss, schist and granite. This research is aimed at assessing the geochemical characteristics of pegmatite in the Ogodo-Odobola area to evaluate their rare metal potential. Field investigation was undertaken to determine the occurrences and relationships of the pegmatites with the host rocks. Thirty-three (33) fresh pegmatite samples were analysed using X-Ray Fluorescence (XRF), Inductively Coupled Plasma Optical Emission Spectrometry (ICP OES) and Inductively Coupled Plasma Mass Spectrometry (ICPMS) techniques at the National Geoscience Research Laboratory, Kaduna and the Activation Laboratories Ltd. (Actlab), Ontario, Canada respectively. Major oxides in the whole rock pegmatite show that they are of siliceous (SiO2; 72.82 wt.% average) and peraluminous (Al2O3; 16.78 wt.% average) composition. The K2O, Na2O and Fe2O3 contents average 4.81 wt.%, 3.13 wt.% and 1.27 wt.% respectively while CaO, MnO, MgO, TiO2 and P2O3 are each less than 1.0 wt.%. Average values of trace elements in the pegmatite are Ta (12.40 ppm), Sn (18.36 ppm), Nb (94.51 ppm), Be (16.14 ppm), Rb (480.23 ppm), U (12.47 ppm), Cs (17.14 ppm), Ga (39.91 ppm), Ge (3.91 ppm), W (4.81 ppm), Li (40.98 ppm), Mn (890 ppm) and B (18.96 ppm). Ratios of diagnostic elements of K/Rb (75.21 ppm), K/Cs (3348.39 ppm), Rb/Sr (25.55 ppm), Rb/Cs (37.18 ppm), Ta/W (2.78 ppm), Nb/Ta (8.81 ppm), Ba/Rb (0.07 ppm) indicate a moderate index of fractionation. A/CNK >1 and Al2O3>CaO+Na2O+K2O with enrichment of SiO2, Al2O3, Na2O, K2O and depletion of Fe2O3, MnO and MgO suggests that Ogodo-Odobola pegmatite is of peraluminous bulk composition and plots of A/NK versus A/CNK and Rb versus (Y+Nb) discriminates the pegmatite in the peraluminous Lithium-Caesium-Tantalum (Li, Rb, Cs, Be, Ga, Nb Ta, Sn, B, Ge, U, W) of syn-collisional to within plate granitic family. The plots of Ta versus Cs, Ta versus Ga, Ta versus (Cs+Rb) and Be versus K/Nb, with over 70 % of the samples plotting below the Beus line and 100 % below the Gordiyenko line reveal that the pegmatites from the study area are barren to marginally mineralized in rare metals (Ta>Sn>Nb). Keywords: Pegmatite, Siliceous, Peraluminous, Rare metal, Syn-collisional
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    Exploration of Groundwater within the Mariam Babangida Girls Science Secondary School Minna, NorthCentral Nigeria Using Schlumberger Vertical Electrical Sounding Techniques
    (Journal of Science, Technology, Mathematics and Education (JOSTMED), 2012-08) Momoh, O. L.; Amadi, A. N.; Abdulfatai, I. A.; Omanayin, Y. A.; Onoduku, U. S.; Onah, M.
    A Geoelectrical investigation adopting Schlumberger vertical electrical sounding (VES) have been carried out to explore for groundwater within the premises of Mariam Babangida Girls Science Secondary School, Bosso, Minna, Niger State. This is with a view of to resolve the problem of acute water shortages experienced by the staff and students of the institution. The area lies within the basement rock complex of North Central Nigeria with biotite granite and muscovite granite constituting the main lithological units. The survey was carried out using ABEM SAS 300C Terrameter along five (5) established traverses with 40 m maximum electrode separation. The VES data were analyzed and interpreted through curve matching and the use of Resist software to obtain the geoelectric parameters. These were used in constructing the 1D geoelectric sections and the isopach map. The geoelectric sections revealed the presence of four geo-electric layers namely the top soil, the weathered layer, the partly weathered/fractured bedrock and the resistive bedrock. The contoured depth to bedrock contour map reveals a significant linear feature delineated by the VES as fractures beneath T2V7, T2V8 and T3V9 and is filled with clayey substratum except T3V9 that are characterized by clayey sand materials. T3V9 is therefore recommended for drilling and groundwater development to a depth of about 30 m. however, the groundwater potential of the study area is generally low.
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    GEOLOGY AND GEOCHEMISTRY OF PEGMATITES OF OGODO – ODOBOLA, NORTH CENTRAL NIGERIA: A STATUS REVIEW
    (FUDMA Journal of Sciences (FJS), 2022-12) Omanayin, Y. A.; Waziri, N. M.; Onoduku, U. S.; Alabi, A. A.; Amadi, A. N.
    Pegmatites are an extremely, coarse-grained igneous rocks of granitic composition, constituting of mainly large crystals of quartz, feldspar and mica. Their occurrence cut across various formations, but mostly around granitoids. They are known to host industrial, rare metals, exotic minerals and gemstones of economic value. Due to the continuous demands and recently discovered uses of some of these minerals, its continuous exploration can never be over-emphasized. Pegmatites occurrence in Nigeria were formerly confined to certain quadrants but resent research has proved they also exist in other zones too. Its occurrence in Ogodo-Odobola area is a recent discovery with scantily available literature. The Few available research work conducted on pegmatite of the Ogodo-Odobola area in Kogi State, North central Nigeria has been reviewed. The works focused on its feldspar content for economic value and the latter attempted the mineralization potential of the pegmatites. The area is revealed to be underlain by schistose and granitic lithologies and intruded by the pegmatite dykes of various dimensions. However, recent studies on granitic pegmatites have evolved just as the pegmatites, not only concentrating on their industrial potentials but also on rare metal mineralization potentials which presently are a key to unlocking the future technologically. A few of those relevant and recent studies in the field were also reviewed to bring forth new ways of dealing with this present world cake to geoscientists. White micas are a useful mineral for determining the degree of evolution in pegmatites. This was achieved in the research work using K/Rb ratios paired with incompatible elements such as Cs. Decreasing K/Rb and increasing Cs is a signs of increasing evolution. The modeling of fractional crystallization of white micas in pegmatites using these trace elements determined that the pegmatites are a result of 99% to 99.99% crystallization of a granitic melt. Keywords: Pegmatites, Ogodo-Odobola, White Mica, Kogi State, North Central, Nigeria
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    Hydrogeochemical Analysis and Potential Pollutant of Water Resources Around Ajaokuta Steel Complex, North Central, Nigeria
    (Journal of Geography and Earth Sciences, 2014-06) Mamodu, A.; Onoduku, U. S.; Ako, T. A.; Abraham, S. U.; Amadi, A. N.; Omanayin, Y. A.
    The citing of Ajaokuta steel complex near its major raw materials (Iron) has brought about economic development in Kogi State, Nigeria. As a result of poor management of industrial waste, the only River where most people in the community get their drinking water became polluted. The aim of this research is to determine the quality of water and its pollutant within the study area. In order to meet the objective of the research, both physical and hydrogeochemical analysis were carried out. The physical parameters determined indicated (on average), a Ph of 7.44, temperature of 27°C, electrical conductivity of 106.8us/cm and turbidity of 157.4 NTU. 20 water samples were analyzed using Flame analysis photometry and Atomic absorption spectrophotometer.The result reveals on the average: 1.227mg/l Na+ , 2.3 mg/l K+ , and 2.545mg/l Ca2+2.6mg/l NH4+ , 0.17mg/l Cu 2+ , 0.45mg/l Fe2+ , 0.4mg/l Cr3+ , 0.06mg/lMn2+<10, ug/l As3 . . There were gradual decreases in concentration in some elements as one move further away from the steel complex (inferred source of pollution). The reason for these decreases maybe due to distance from the source of pollution and seepage into the groundwater. Iron and manganese were found to be very higher when compared to World health standards. Dangote group of Company’s E.I.A report also shows higher concentration of Fe2+, Mn2+and Cu2+in plant tissue. Therefore, the research concludes that Fe2+ and Mn2+ were the main pollutants while a Cu 2+andCr3+arethe minor pollutants of water resources in the study area. The research also, preliminary concludes that poor handling of industrial waste may have contributed majorly to the pollution of water. Keywords: Ajaokuta, water, hydrogeochemical analysis, pollutant, Environmental Impact Assessment (E.I.A), industrial waste, Atomic absorption spectrophotometer
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    Preliminary Studies of Pegmatites of Ogodo-Odobola area of Idah Sheet 267NW, North-Central Nigeria
    (6th International Faculty of Science Conference Book of Abstract, Federal University Oye-Ekiti, Ekiti State, Nigeria, 2023) Omanayin, Y. A.; Waziri, N. M.; Onoduku, U. S.; Alabi, A. A.
    Pegmatites in the world over have been acknowledged to serve as host to lots of minerals (industrial, ore and gemstones). Recently, there is an upsurge in the interest for pegmatite deposits due to the newly discovered important uses of lithium ores among others. The granitic pegmatite of Ogodo-Odobola in Ajaokuta, Central Nigeria belongs to the pegmatite belt of North-Central Nigeria that has received very little attention and consequently, yet to be well studied. Therefore, detailed geological field mapping of the pegmatites and host rocks aimed at understanding their mode of occurrence and field relationship and to assess their mineralization potentials was conducted. The methods employed for this study include both geological fieldwork and laboratory analysis. Twelve (12) representative samples were selected for petrographic analysis. Geological fieldwork shows the study area is underlain by migmatite gneiss, schist, with intrusions of granite and pegmatite. The pegmatites occur in tabular form with varying widths and lengths. Principal joint directions show NNE-SSW direction which is believed to have influenced the pegmatite emplacement. Petrography of the representative rock samples reveal an average mineralogical composition of hornblende, biotite, quartz, plagioclase, microcline, muscovite, myrmekite and opaque minerals for the host rocks. While microcline, plagioclase, muscovite, biotite, and accessory and opaque mineral for the pegmatites. The pegmatite of the study area is worth probing as the results have shown prospect for possible economic minerals. Keywords: Mineralization, Lithium Ores, Structural Features, Petrography, Ajaokuta