In this study, samples from five different marble deposits, all within the area underlain by the schist belt in the Ukpilla area of Edo State (Nigeria), were subjected to standard
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OBAJANA MARBLE DEPOSIT IN THE PRECAMBRIAN BASEMENT COMPLEX OF CENTRAL NIGERIA 1 A. A., 1 A. O. and 2 O. K. 1Department of Geology, University of Ibadan, Ibadan, Nigeria 2Department of Geological
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X- Ray Fluorescence (XRF) Spectrometric analysis of whole rock samples to determine the major elements composition of the marble deposit was carried out. Major element oxides determined include SiO2, CaO, MgO, Al2O3, Na2O, K2O, SO3, and total Fe as Fe2O3. Loss on ignition (L.O.I) of the marble samples was determined gravimetrically.
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Limestone occurs only in the sedimentary basins in Nigeria. It occurs mainly in the Benue Trough (Lower, Middle and Upper), Sokoto, Dahomey and Borno (Chad) Basins. Limestone-forming environments (shallow coastal marine conditions), appear to have occurred several times in the geological history of the basins. However, the limestone deposits of the
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· Detailed geological and geophysical studies have been carried out on the Jakura marble deposit in Kogi State (Okunlola, 2001, Jatau & Bajeh, 2008, Ikpeshi marble deposit in Edo State (Odeyemi et
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· Geochemical analyses of the marble using inductively coupled plasma-atomic emission spectrometry (ICP-AES) and inductively coupled plasma-mass spectrometry (ICP-MS) reflect the calcitic (CaO 53.39
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SCALE: 1: 650,000 FIG 1: MAP OF FCT SHOWING LOCATION OF THE STUDY AREA. Beltaro, (1968) carried out an investigation of an area south of Burum and found additional five more deposits – Taka – Lafia East and West, Kasada and Kusaki North and South. He found that all the deposits have similar chemical compositions (55.7, CaCO3 and
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ORIGINAL PAPER Quality and durability of some marble deposits in the southern schist belt (Nigeria) as construction stones O. P. Aghamelu1 • J. I. Amah1 Received: 16 March 2016/Accepted: 12 September 2016/Published online: 21 September 2016 Springer
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This paper investigates and reports the lithological and compositional features of Igue marble deposit in southwestern Nigeria. The deposit occurs as low-lying
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In various districts in Nigeria, marble bodies are Nigeria. being These bodies are commonly associated with the Schist Belts (Fig.1), which may be regarded as infolded
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PDF | On May 24, 2022, Ayodele Daniel and others published a-preliminary-estimate-of-the-reserve-of-the-marble-deposit-in-itobe-areacentral-nigeria-2329-6755-1000216 | Find, read and cite all the
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· The VES data obtained were interpreted using ipi2win Software. The results showed three layers indicating subsurface geologic sequence probed 26.4 m and beyond with clay/clayey sand (23.3 – 219.1 Ωm), sand (423-2040 Ωm) and marble (12661-404498 Ωm). The occurrence of marble deposit was revealed at VES points at 1, 2
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· some viable marble deposits in Nigeria have also been reported (Okunlola et al., 2015; Dakus et al., 2017; Abdullateef et al., 2014; Adedoyin et al., 2017). Furthermore, resent publications on marble deposits around Igarra area include Obasi Agomuo (2016
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www.theinternationaljournal.org > RJSITM: Volume: 01, Number: 12, October-2012 Page 23 Economic evaluation of Burum-Takalafia marble deposit, Federal Capital Territory, Abuja, Nigeria Ako Thomas
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Ife Journal of Science vol. 17, no. 3 (2015) COMPOSITIONAL CHARACTERISTICS AND FUNCTIONAL APPLICATIONS OF OBAJANA MARBLE DEPOSIT IN THE PRECAMBRIAN BASEMENT COMPLEX OF CENTRAL NIGERIA 1 A. A., 1 A. O. and 2 O. K. 1Department of Geology, University of Ibadan, Ibadan, Nigeria
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Geochemical investigations of the marble deposit in Itobe, Kogi state, central Nigeria shows that the two outcropping masses (mass I and mass II) of the marble deposit are calcitic in composition. The two masses of the marble deposit may have been deposited in shallow structural basins, and mass I with a much higher MgO content (10.4%) was
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some viable marble deposits in Nigeria have also been reported (Okunlola et al., 2015; Dakus et al., 2017; Abdullateef et al., 2014; Adedoyin et al., 2017). Furthermore, resent publications on marble deposits around Igarra area include Obasi Agomuo (2016
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：4 Marble Deposits-In Nigeria, Africa, and globally, marble has a wide range of industrial applications, it is extensively deposited throughout the country but is majorly found in Abuja (FCT), Katsina, Oyo, Benue, Kogi, Kwara,
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· Marble is a metamorp hosed lim estone. Limestone and marble are carbonate rocks, dominated by the. mineral calcite (CaCO. ). Nigeria is endowed with large deposits of limestone and marble loc ated
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This article summarizes the information available on the country’s limestone and marble deposits (the geology, occurrences, characteristics, reserves, production and quality). Recommendations are proposed for developing the limestone and marble industry to make a positive contribution to the national economy.
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：5 Nigeria is endowed with large deposits of limestone and marble located in all parts of the country. The limestone at Mfamosing, near Calabar, is the largest and the purest deposit
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Abstract. The determination of the impacts of marble mining on the environment in Igarra was carried out via the analysis of soil and water samples as geological medium. Seven soil samples, ten
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Marble deposits occur prominently in Igarra and Ikpeshi areas of Southwestern Nigeria. Forty marble samples were subjected to geochemical and physical analysis in order to
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One sample each was taken from the snow-white marble (IGRR_2_15) and the dark-grey marble (IGRR_2_42) layers at depths of 15 m and 42 m respectively. BH-3 was drilled to 53 m depth. The subsurface
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· 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
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· Igbeti, Ososo and Jakura marble deposits in South-western Nigeria. J. Min. Geol. 31(1) pp 89 – 96. 16. Emofurieta, W.O., Imeokparia The marble deposit is characterised by both local
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Nigeria is endowed with large deposits of limestone and marble located in all parts of the country. The limestone at Mfamosing, near Calabar, is the largest and the purest deposit in Nigeria. It is about 50 metres thick at the quarry site. West of Calabar, another
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· The deformed, low-grade, metasedimentary-volcanic schist belts of NW Nigeria, and the voluminous granitoid plutons which invaded them, are expressions of late Proterozoic-early
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ON THE GENESIS OF NSOFANG MARBLE OF IKOM AREA OF SOUTHEASTERN NIGERIA. and Ukwang E. E. Department of Geology, University of Calabar, P. M. B. 1115 Calabar – NIGERIAABSTRACT: Physical, petrographical and geochemical data are used to constrain the mode of fo. ation of low grade marble occurring in Nsofang and environs,
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This paper investigates and reports the lithological and compositional features of Igue marble deposit in southwestern Nigeria. The deposit occurs as low-lying heterogeneous units under a humus-laden dark brown tropical soil within Igarra Schist Belt on south eastern flank of basement complex of southwestern Nigeria.
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