尼日利亚西北部Tandama地区Malumfashi片岩地球化学特征及岩石成因

Idzi Alaku, O. Moshood, A. Agbor, A. Amos
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引用次数: 3

摘要

Malumfashi片岩与混辉片麻岩和黑云母花岗岩伴生,约占尼日利亚西北部Tandama地区的60%。Na 2o /Al 2o3、微量元素比值Th/U和REE等地球化学特征表明,原岩主要来源于长英质火成岩。构造上,sio2 / al2o3与k2o / na2o对比图显示原岩在被动边缘环境中演化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geochemical Characteristic and Petrogenesis of Malumfashi Schist around Tandama Area, North-Western Nigeria
between designed the study, the statistical ABSTRACT Malumfashi schists which occur in association with migmatite-gneisses and biotite granite, occupy about 60% of Tandama area, north-western Nigeria. geochemical features like the Na 2 O/Al 2 O 3 values, trace element ratios such as Th/U and REE patterns suggest that the protolith are predominantly derived from felsic igneous sources. Tectonically, SiO 2 /Al 2 O 3 versus K 2 O/Na 2 O plot revealed the protolith to have evolved within passive margin environment.
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