The mafic and ultramafic rocks of southwest Obudu, Nigeria are located within the Paleoproterozoic granulites facies rocks of the Bamenda Massif. These mafic and ultramafic rocks were not subjected to high level deformation and metamorphism which the surrounding rocks experienced...
Open access
Research Article10.9734/JGEESI/2016/25536
Very little research has been carried out and reported on the Irruan granitoids. Geological field mapping and laboratory analyses were carried out to ascertain the petrological, geochemical and structural attributes of the Irruan Basement Rocks in southern Obudu Plateau, southeas...
Strain has been analyzed from the metamorphic spots within deformed schist and phyllite in the Igarra schist belt, southwestern Nigeria. Strain magnitudes were obtained by using the graph of length against width of spots, Harmonic mean (H), and the Rf/ø technique. The values of s...
Open access
Research Article10.9734/ACRI/2016/30937