Petrological Features and Geochemical Characterization of Igneous Rocks in Ado-Ekiti, Southwestern Nigeria

Akinola, O. O, Akomolafe, A. D., Madukwe, H. Y.
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Abstract

This research investigates and report petrological features and geochemical characteristics of igneous rocks in Ado-Ekiti, Southwestern Nigeria. Exhaustive geological fieldwork reveals Ado-Ekiti is underlain by migmatite-gneiss, quartzite, granite (porphyritic and fine-grained) and charnockite. Petrographic investigation revealed overwhelming presence of quartz, biotite and plagioclase in all the rocks while microcline and opaque minerals occur in subordinate amounts. Average SiO2 content in porphyritic granite (74.56 %) is marginally higher than charnockite (73.51%) and fine-grained granite (70.41%). These values correlate well with previous works in the study area and agrees with similar rocks in other parts of the country. Analytical results using Phillips Panalytical PW1480 X-ray Fluorescence Spectrometer with Rhodium Tube as the X-ray source revealed the siliceous nature of the rocks. The binary plot (Na2O+K2O) vs SiO2 established the rocks are granitic with all the samples plotting within granite field. AFM ternary diagram shows the rock have calc-alkaline affinity. Geochemical classification by (Na2O + K2O-CaO) vs SiO2 diagram reveals the rocks are “Calc-alkalic and calcic”. The elevated K2O (average of 4.41%) in the data signaled High-K calc-alkaline type on K2O vs SiO2 binary diagram. Alumina Saturation Index (ASI) showed the rocks are metaluminous while Al2O3 / (Na2O + K2O) vs Al2O3/ (Na2O +K2O +CaO) plot suggest the rocks have mantle origin
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尼日利亚西南部Ado-Ekiti地区火成岩岩石学特征及地球化学特征
研究报告了尼日利亚西南部Ado-Ekiti地区火成岩的岩石学特征和地球化学特征。详尽的地质野外调查显示,Ado-Ekiti的下垫层为混杂岩片麻岩、石英岩、花岗岩(斑岩和细粒)和绿帘岩。岩石学调查显示,石英、黑云母和斜长石在所有岩石中占绝大多数,微斜长石和不透明矿物次之。斑岩花岗岩SiO2平均含量为74.56%,略高于绿绿岩(73.51%)和细粒花岗岩(70.41%)。这些值与研究地区以前的工作相吻合,并与该国其他地区的类似岩石相一致。采用Phillips Panalytical PW1480 x射线荧光光谱仪,以铑管为x射线源,分析结果揭示了岩石的硅质性质。Na2O+K2O / SiO2二元图确定岩石为花岗质,所有样品均在花岗质范围内。AFM三元图显示岩石具有钙碱性亲和关系。地球化学分类(Na2O + K2O-CaO) vs SiO2图显示岩石具有“钙碱性和钙性”特征。在K2O / SiO2二元图上,数据中K2O升高(平均为4.41%)为高钾钙碱性。Al2O3/ (Na2O +K2O)与Al2O3/ (Na2O +K2O +CaO)比值图表明岩石具有幔源性
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