尼日利亚西南部的伟晶岩-片麻岩-花岗岩基底:矿物学和地球化学证据表明可能存在共同的古代原岩

Olusola A OlaOlorun, Oluwatoyin O Akinola
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引用次数: 0

摘要

尼日利亚位于泛非造山带南段,岩浆岩-片麻岩-花岗岩地形是其基底复合体的主要组成部分。对尼日利亚西南部 Idanre 地区的这一岩石单元进行了野外地质学、光学矿物学和地球化学研究,以确定其特征、阐明其构造意义并确定其起源。主要元素、痕量元素和稀土元素(REE)的组成分别在加拿大温哥华的必维国际检验集团通过 XRF 和 ICP-MS 技术进行了测定。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Migmatite-Gneiss-Granite Basement of Southwestern Nigeria: Mineralogical and Geochemical Evidence for a Possible Common Ancient Protolith
Nigeria occupies southern section of the Pan-African orogenic belt and migmatite-gneiss-granite terrain forms a major component of its basement complex. Field geology, optical mineralogy and geochemical study of this rock unit in Idanre area, SW Nigeria were undertaken with a view to characterize them, elucidate their tectonic significance, and determine their origin. Major, trace and Rare Earth Elements (REE) composition were determined by XRF and ICP-MS techniques respectively in Bureau Veritas, Vancouver, Canada.
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