Subsurface mapping and geochemical investigation of a marble deposit around Igarra, Southwestern Nigeria

O. Oluwajana, A. Ogunyele, J. Egunjobi, A. Ajayi
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Abstract

Subsurface mapping of a marble deposit around Igarra and geochemical analysis of seven marble samples collected at different depths in four drill holes were carried out with the aim of determining the chemical compositions and economic viabilities of the deposit. Subsurface mapping and lithologic description revealed that snow-white and grey to dark grey marble layers occur in the four drill holes. Results of the geochemical analysis show that the CaO and MgO contents of the snow-white marble samples retrieved from depths between 10 m and 20 m (43.90-48.90 wt. % and 0.19-2.35 wt. % respectively) reflected calcitic to fairly dolomitic nature of the marble samples. This is confirmed by the high CaCO3 (91.65-95.75 wt. %) content of the samples. Grey to dark grey marble samples taken from depths between 30 m and 48 m have moderately high CaO contents (44.00-52.60 wt. %) and significantly high MgO contents (3.50-8.70 wt. %) which makes them highly dolomitic and impure. The pure, calcitic to fairly dolomitic marble is considered suitable as raw material for Portland cement production, flux in steel making and for paper production while the impure, dolomitic marble is suitable for making dimension stones and structural wares for landscaping purpose.
尼日利亚西南部伊加拉附近大理石矿床的地下测绘和地球化学调查
对伊加拉附近的大理石矿床进行了地下测绘,并对四个钻孔在不同深度采集的7个大理石样品进行了地球化学分析,目的是确定该矿床的化学成分和经济可行性。地下填图和岩性描述显示,4个钻孔均发育雪白、灰色至深灰色大理岩层。地球化学分析结果表明,10 ~ 20 m深度的雪白大理岩样品的CaO和MgO含量(分别为43.90 ~ 48.90 wt. %和0.19 ~ 2.35 wt. %)反映了大理岩样品的方解石-白云石性质。样品的高CaCO3 (91.65-95.75 wt. %)含量证实了这一点。从30米至48米深度的灰色至深灰色大理石样品具有中等高的CaO含量(44.00-52.60 wt. %)和显著高的MgO含量(3.50-8.70 wt. %),这使它们具有高白云质和不纯性。纯的、方解质到相当白云质的大理石适合作为硅酸盐水泥生产、炼钢助熔剂和造纸的原料,而不纯的、白云质的大理石适合制作尺寸石和用于园林绿化的结构制品。
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