Answers are grounded in this paper and cite their sources.
The understanding of the structural complexity and development of the Ifewara- Zungeru strike slip fault with other associated tectonic features, such as the Mega Oreke-Okegbo and Okemesi fold, the doubly plunging fold structures and the adjacent thrust belt is yet to be appraised in any publication. These features extend over an area of more than 800 square km and the different aspects of such regional intraplate strike-slip fault and associated structures are fully comprehended with Google Terrain Map and aeromagnetic data interpretation. This study aims to elucidate the critical structural relationships and overprinting relationships influencing the occurrence of the regional strike-slip faults, the folds and the thrust systems. The research provides detailed structural information about the mega Oreke-Okegbo fold and the adjacent thrust duplexes. The former was simply referred to as a shear zone, while the thrust duplexes have not been fully described in terms of nature and implication. The research proposes to produce illustrations and data compilations that will contribute to our knowledge of these structures and the potentiality of the associated mineral resources in this area.
No takes yet. Share an insight, caveat, or question.
Oluseyi Adunola Bamisaiye (2024) studied this question.
Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context: