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Geology, Geochemistry and Petrogenesis of Precambrian Rocks of Part of Sheet 244 of Ado-Ekiti, Southwestern Nigeria

机译:尼日利亚西南部Ado-Ekiti 244页的部分前寒武纪岩石的地质,地球化学和岩石成因

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The geology, geochemistry and petrogenesis of Precambrian rocks of part of sheet 244 (Ado-Ekiti), Southwestern Nigeria is reported in this paper. The study area was mapped systematically and the lithologies encountered include migmatite gneiss, granite gneiss, older granite, and charnockite. The various structures mapped on the outcrops are compositional banding, pinch and swell structures, joints, xenolith inclusions among others. The gneisses cover the largest proportion (≈60%) of the study area while the Older granites and charnockites cover the North Eastern and Southwestern part of the area. Six fresh samples of rocks were analysed for petrographic study while another six representative samples (2 per rock type) were also analysed for geochemical composition using Atomic Absorption Spectroscopy. The petrographic study reveals the dominance of quartz, biotite, plagioclase and microcline in the thin sections for the different rock types. The geochemical analyses of the rocks show in percentage average SiO 2 compositionof 67.63 in charnockites, 67.09 in granites and 67.99 in gneisses. Alumina varied from 13.77% in the charnockites, and the lowest in the gneisses with 12.91%.The high percentage composition of SiO 2 obviously indicate siliceous nature of all the rock units in the area with low content of Fe 2 O 3 and MgO as well as various discriminatory diagrams establishing a common petrogenetic origin related to igneous material source.
机译:本文报道了尼日利亚西南部244页(Ado-Ekiti)的部分前寒武纪岩石的地质,地球化学和岩石成因。对研究区域进行了系统地制图,所遇到的岩性包括:辉长岩片麻岩,花岗岩片麻岩,较老的花岗岩和菱镁矿。映射在露头上的各种结构包括组成带,夹缩结构,接头,异物包裹体等。片麻岩覆盖了研究区域的最大部分(约60%),而较老的花岗岩和霞石岩覆盖了该区域的东北和西南部分。分析了六个新鲜的岩石样品以进行岩石学研究,同时还使用原子吸收光谱法分析了另外六个代表性的样品(每个岩石类型两个)的地球化学组成。岩石学研究表明,对于不同类型的岩石,石英,黑云母,斜长石和微斜岩在薄片中占主导地位。岩石的地球化学分析显示,平均SiO 2百分含量分别为霞长岩中的67.63,花岗岩中的67.09和片麻岩中的67.99。铝的含量在方铁矿中为13.77%,在片麻岩中最低,为12.91%.SiO 2的高百分比组成显然表明,Fe 2 O 3和MgO含量也较低的地区所有岩石单元均为硅质质作为各种鉴别图,建立了与火成岩物质来源有关的常见成岩成因。

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