
The Manyoni–Singida Gold Project is located within the Moyowosi–Manyoni Greenstone Belt of the Dodoma Superterrane, representing a large, underexplored frontier terrain with emerging potential for structurally controlled gold systems.
Although much of the belt is masked by transported regolith and proto-lacustrine sediments, high-resolution geophysics and limited drilling have confirmed elongated granitoid bodies with mafic inclusions and structurally bounded basement domains—features consistent with deep-seated fluid pathways and concealed mineral systems.
Importantly, the Moyowosi–Manyoni Superterrane remains comparatively underexplored for gold relative to Tanzania’s Archean greenstone belts, creating an opportunity for modern, technology-led exploration focused on:
