Home|Journals|Articles by Year|Audio Abstracts
 

Original Research

Nig. J. Basic Appl. Sci.. 2017; 25(2): 87-99


PETROGRAPHY AND GEOCHEMISTRY OF ROCKS OF NORTHERN PART OF WONAKA SCHIST BELT, NORTHWESTERN NIGERIA

Aliyu Abdu Ibrahim, Muhammed Abdullahi Usman.




Abstract

ABSTRACT
Systematic mapping and sampling of rocks of northern part of Wonaka schist belt on a scale of 1:50,000 shows that belt is composed of gneiss, granite gneiss, muscovite-biotite schist, banded iron formation, amphibolite, granite, granodiorite and diorite as major rock types, other rocks are aplite, and pegmatite. Petrographic and geochemical data shows that the there are two types of gneisses in the area: the orthogneiss and the paragneiss. Plots of TiO2 vs SiO2 shows that the granite gneiss is paragneiss while the gneiss is an orthogneiss. The granites and the granodiorite are I – Type and the amphibolite is volcani-clastic. The banded iron formation (BIF) is shown to be hematite facies type from a plot of MnO vs FeO(T). It can therefore be said that the orthogneiss represents the original basement rock possibly dating back to the early phase of the Eburnean orogeny. At later stages of the Eburnean, sedimentary deposition and subsequent metamorphism of the sediments might have led to the formation of the paragneiss and the metasediments with the associated BIF as indicated by the REE distribution pattern. The NNE – SSW and the N – S structural trends on the rocks might have been developed by the over printing effects of the Pan – African orogeny.

Key words: orthogneiss, schist belt, paragneiss, banded iron formation, metasediments






Full-text options


Share this Article


Online Article Submission
• ejmanager.com




ejPort - eJManager.com
Refer & Earn
JournalList
About BiblioMed
License Information
Terms & Conditions
Privacy Policy
Contact Us

The articles in Bibliomed are open access articles licensed under Creative Commons Attribution 4.0 International License (CC BY), which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.