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Mineralization of pegmatites in parts of the Oban Massif, Southeastern Nigeria: A preliminary analysis

Kingsley A.Ero Ekwueme Barth N.

中国地球化学学报(英文版)2009,Vol.28Issue(2):146-153,8.
中国地球化学学报(英文版)2009,Vol.28Issue(2):146-153,8.DOI:10.1007/s11631-009-0146-2

Mineralization of pegmatites in parts of the Oban Massif, Southeastern Nigeria: A preliminary analysis

Mineralization of pegmatites in parts of the Oban Massif, Southeastern Nigeria: A preliminary analysis

Kingsley A.Ero 1Ekwueme Barth N.1

作者信息

  • 1. Department of Geology, University of Calabar, P.O. Box 3651 Unical Post Office, Calabar, Nigeria
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摘要

Abstract

The Oban Basement Massif of southeastern Nigeria is composed of metamorphosed rocks including phyllites, schists, gneisses and amphibolites cut by pegmatitic dykes of varying length and thickness, which intruded the metamorphic rocks. Preliminary geochemical study and analysis of these pegmatites from western Oban Massif at Uyanga, Akwa Ibami, Iwuru I, Iwuru II and Igbofia showed that the pegmatites are highly albitized. This is inconsistent with earlier postulations that the pegmatites in this part of Nigeria are barren. Indices of fractionation such as Ba/Rb, K/Rb, Na/K, K/Cs, K/Ba reveal that the pegmatites are mineralized and different discrimination plots show that they are enriched in Li, Be, Sn, Ba, Ta, Ni, Cs, Sn and Zn. Rare metal indicative elements such as Ta, Nb, Rb, Cs, and Sn are enriched in the pegmatites, confirming that the pegmatites are mineralized.

关键词

Precambrian pegmatite/mineralization/Oban Massif/rare-earth element

Key words

Precambrian pegmatite/mineralization/Oban Massif/rare-earth element

分类

天文与地球科学

引用本文复制引用

Kingsley A.Ero,Ekwueme Barth N...Mineralization of pegmatites in parts of the Oban Massif, Southeastern Nigeria: A preliminary analysis[J].中国地球化学学报(英文版),2009,28(2):146-153,8.

基金项目

The authors appreciate Dr. Bassey Ephraim of the Department of Geology, University of Calabar, Nigeria, for his assistance with field work, logistics and sample preparation. The contribution of Mr. E. E. Ukwang to interpretation is also acknowledged. This paper is the outcome of a postgraduate diploma project by Ero K.A. supervised by Prof. Ekvueme B.N. ()

中国地球化学学报(英文版)

2096-0956

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