The Eastern Nigeria terrane belongs to the 3000 km-long Trans-Saharan belt which was
formed in the Neoproterozoic, between 750 and 500 Ma by continental collision between the …

Orientations of planar, linear and micro-structures are consistent with the results of isotopic
data from the Uwet area of southeastern Nigeria which indicate that the area was subjected …

The present research paper reveals the occurrences of metachaotic rocks/accretionary
sediments (mélange) in Igarra, southwest Nigeria. These metachaotic rocks are associated …

Abstract The Oban Massif forms part of the Precambrian to Early Paleozoic Nigerian
basement complex and predominantly consists of metasediments, granodiorites, granites …

Abstract The Nigerian Basement Complex has undergone polyphase deformation and
polycyclic metamorphism during the Proterozoic and early Phanerozoic periods. Andalusite …

Barite deposits occur mostly as concealed mineralization dominantly in shales and
sandstones of Cretaceous age in Cross River State. Vertical Electrical Sounding (VES) and …

The determination of the mineralogical composition of rocks that underlie Okom-Ita area, in
Oban Massif became necessary for the interpretation of the petrogenesis and protoliths of …

In this work, seismic refraction was used to obtain elastic properties (shear modulus (μ),
Young modulus (E), Bulk modulus (K) and lithological information in Uyo and its environ as …

Metasediments comprising phyllites, schists and gneisses constitute the predominant rock
types in Uwet area of the Oban Massif of southeastern Nigeria. These rocks which range …

Abstract Cross River State is composed of sedimentary rocks which constitute the Calabar
Flank and metamorphic and intrusive rocks which crop out in the Oban massif and Obudu …