INDEPENDENT GEOLOGIC FIELD MAPPING OF THE IGARRA AXIS OF THE BASEMENT COMPLEX
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ABSTRACT
The focus of this study revolves around independent geologic field mapping of the igarra axis of the basement complex. Basically, geological mapping involves the study of rocks; in situ, that is, in their natural environment and the representation of such rocks on a geological map. Furthermore, rocks of the Igarra area constitute part of the Basement Complex of southwestern Nigeria. This comprehensive report consist of two section A and B. Although section A is also the basement complex of Nigeria consists of the migmatite gneissic complex, the metasediment, schist belt, the granitoids and the minor rocks. The result of the detailed geologic mapping of the area has shown that more than one rock type is present in the region compare with the previous work, the rock present in the area according to the field mapping are four which include granite, migmatite, quartzite and granite gneiss. Magnetic investigation of the study area was also carried out with the aim of delineating the lithological units and the geologic structures in the area. The study therefore recommends that For geological field mapping to be carried out efficiently, it is essential that proper planning is executed. Moreso Measurements must be performed meticulously and, if necessary, more than once for confirmation purposes.
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