尼日利亚乔斯高原新花岗岩省一些锡石的矿物学和地球化学特征

M.I. Ogunbajo
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引用次数: 0

摘要

从矿物学、颜色变化和化学角度对乔斯高原四个不同冲积矿区的锡石进行了研究。入射光显微研究显示的每种颜色的光学性质,加上电子探针分析显示的化学成分的变化,表明锡石是在不同的物理化学条件下结晶的。有些品种(黑色品种)是高温品种,而其他品种,即红色和白色品种是低温品种。此外,这些锡石的化学成分倾向于支持年轻花岗岩的年龄迁移,即北部锡石比南部锡石更古老,SnO2含量更丰富,Fe、Nb和Ta元素含量更低。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The mineralogy and geochemistry of some cassiterite from the Younger Granite province of the Jos Plateau, Nigeria

Cassiterite from four different alluvial mining localities on the Jos Plateau were investigated from the point of view of their mineralogy, colour variety and chemistry. The optical properties of each of the colour varieties as revealed by the incident light microscopic studies coupled with the variation in their chemical composition as revealed by the electron microprobe analyses indicate that the cassiterites crystallized under different physicochemical conditions. Some (black varieties) are high temperature forms, whereas others, i.e., the red and white varieties are low temperature forms. Furthermore, the chemistry of these cassiterites tends to support the age migration of the Younger Granites whereby the northern cassiterites tend to be older, richer in SnO2 and poorer in the elements Fe, Nb and Ta than the southern cassiterites.

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