尼日利亚中部Idah Sheet 267NW Ogodo-Odobola地区伟晶岩特征

Y. A. Omanayin, N. M. Waziri, U. S. Onoduku, A. A. Alabi
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摘要

尼日利亚中部Ajaokuta附近Ogodo-Odobola地区的伟晶岩属于尼日利亚中部伟晶岩带。对伟晶岩和寄主岩进行了详细的地质填图,目的是了解它们的赋存方式和场关系,并评估它们的成矿潜力。选取了12个具有代表性的岩石样品进行岩石学分析。结果表明,该区下覆混辉片麻岩、片岩,花岗岩、伟晶岩侵入。伟晶岩呈板状,宽度(2厘米- 6米)和长度(12 - 200米)不等。主要的联合方向为北北东—南南西,认为这影响了伟晶岩的侵位。典型岩石的岩石学特征为:黑云母(23.90%)、微斜长石(22.15%)、角闪石(15.05%)、石英(10.65%)、斜长石(10.35%)、白云母(8.00%)、金缕石(0.20%)、不透明矿物及副矿物(9.70%)。伟晶岩以微斜长石、斜长石为主,其次为白云母、黑云母、副矿物和不透明矿物。乌戈多-乌多波拉地区伟晶岩具有勘探价值,显示出潜在的经济矿产前景。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Characterization of Pegmatites in Ogodo-Odobola Area of Idah Sheet 267NW, Central Nigeria
The pegmatites of Ogodo-Odobola area around Ajaokuta, Central Nigeria belong to the pegmatite belt of Central Nigeria. A detailed geological mapping of the pegmatites and host rocks was conducted with the aim of understanding their mode of occurrence and field relationship and to assess their mineralization potentials. Twelve (12) representative samples of rocks were selected for petrographic analysis. The results show that the area is underlain by migmatite-gneiss, schist, with intrusions of granite and pegmatite. The pegmatites occur in tabular form with varying widths (2 centimetres – 6 metres) and lengths (12 – 200 metres). Principal joint direction is NNE-SSW which is believed to have influenced the pegmatite emplacement. Petrography of the representative rock samples revealed an average mineralogical composition of biotite (23.90%), microcline (22.15%), hornblende (15.05%), quartz (10.65%), plagioclase (10.35%), muscovite (8.00%), myrmekite (0.20%), and opaque and accessory minerals (9.70%). The pegmatites were found to be dominated by microcline and plagioclase feldspars, and then muscovite, biotite, and accessory and opaque minerals. The pegmatite of the Ogodo-Odobola area is worth probing as the results have shown prospect for possible economic minerals.
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