GEOLOGY AND GEOCHEMISTRY OF QUARZITIC ROCK OF ADO-EKITI SOUTHWESTERN NIGERIA

Student: Olabayo Martins Thomas
Supervisor: Mr Yusuf Abdu-Raheem
HOD: Prof Adeyinka Aturamu
Department of Geology
Science
Ekiti State University, Ado-Ekiti, Ekiti State

Abstract

This study examines the geological and geochemical characteristics of quartzitic rocks in Ado-Ekiti, Southwestern Nigeria, within the Precambrian Basement Complex. These quartzitic formations, predominantly composed of quartz, form significant ridges that provide insights into the geological processes that shaped the region over millions of years. The quartzitic rocks occur as minor yet geologically important units amidst a predominantly gneissic and migmatitic terrain. Typically found in interlayered sequences with other metamorphic rocks, their origins suggest sedimentary precursors subjected to intense metamorphism. This layering indicates a complex geological history marked by sediment deposition and tectonic activity. Geochemical analyses indicate that the quartzitic rocks consist mainly of interlocking anhedral to subhedral quartz grains, characterized by a granoblastic texture. Minor components include feldspar, muscovite, biotite, microcline, and hornblende. The high silica content, often exceeding 90% SiO₂, underscores the quartz- dominated composition. Trace element analysis shows low concentrations of aluminum, iron, magnesium, and calcium, reflecting limited feldspar and mica presence. Distinctive features of the quartz grains, such as undulose extinction and deformation bands, reveal significant tectonic stress impacts throughout their history. Quartzofeldspathic veins observed in the southern study area indicate past intrusive activity, while visible faults and joints highlight geological stresses that have influenced erosion and alteration of the original formations. In conclusion, the quartzitic rocks of Ado-Ekiti represent a transition from sedimentary to metamorphic processes, reflecting the extensive geological events that shaped southwestern Nigeria. Understanding these characteristics enhances knowledge of the region's geological evolution and informs future exploration and resource management efforts. KEYWORDS: Geochemistry, quartzite, metamorphism, tectonic, precambrian

Full-Text Access Notice

In accordance with the NERD Policy on promoting peer-reviewed publication, public access to the full text of a project, thesis or dissertation is restricted for three years, allowing the author and supervisors sufficient time to pursue peer-reviewed publication. During this period, researchers with legitimate academic or research purposes may request authorisation directly from the author to enable NERD to release the indexed full texts of the work using the form below.

Request authorisation from the author