ABOUT US

Imvelo is a dynamic and agile mining corporation strategically situated in West Africa, with primary operations in Nigeria. Our profound comprehension of the local environment, its abundant resources, and the significance of community development, are among the distinctive attributes that define Imvelo. These attributes enable us to effectively manage a diversified assets portfolio encompassing Tin, Copper, Lead, Gold, and Talites. Our mining and exploratory operations are fueled by an unwavering dedication to unearth Africa's wealth of resources while optimising their sustaining value to enrich lives

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Project Kaiama

Imvelo Mining is at the exploratory stage in Kaiama, an under-explored area situated within a region rich in geological potential, which provides exposure to Gold, Copper, Scheelite, Tantalite and other valuable metals.

Kaiama is the provincial capital of Kaiama Local Government Area, situated in Kwara state, within one of the under-explored parts of the North Central Region of Nigeria, covering an approximate area extent of about 770 km2. It is a border town, approximately 60 km from the international boundary between Nigeria and Benin Republic.

Kaiama is readily accessible through the Ilorin-Kishi, the Jebba – Kainji road and Kosubosu Yashika road. While the roads are yet to be fully constructed, there are many untarred rural roads linking the major settlements.Project Kaima capitalises on the region’s rich geological endowment, offering promising prospects for resource exploration and extraction.

Geology

Kaiama area hosts a wealth of mineral resources, including gold, cassiterite, columbite, tantalite, rare earth metals, and gemstones.

Features:

Southwestern Basement Complex of Nigeria, composed of migmatites, gneisses, metasediments, and granites.
Numerous fracture systems, with predominant NE and NW orientations.
Prominent Proterozoic Pan-African granites, indicative of rare earth metals like tin, tantalum, and niobium, typically found within pegmatite formations.
Locally, economic mineral deposits primarily occur within pegmatite and quartz veins

Exploratory Opportunities

Based on interpreted structural maps, the prevailing structural trends in the area encompass NE-SW, N-S, E-W, and NW-SE orientations. NE-SW trends, dominant within the region, are indicative of faults, connecting joints, or shear zones likely formed during regional NW-SE compression, suggesting a favourable direction for ore deposition.