The Joru Prospect represents a large, structurally controlled orogenic gold system located approximately 13 kilometres south of Segele within the Akobo Gold District. Gold mineralisation occurs primarily as quartz‑carbonate vein stockworks hosted within quartz‑feldspathic rocks.
Exploration completed to date, including geological mapping, soil geochemistry, trenching and limited reverse circulation drilling, has confirmed gold mineralisation over a strike length of more than 3 kilometres. Results indicate predominantly low‑grade mineralisation, typically in the range of 1–2 g/t Au, with localised higher‑grade zones interpreted as potential high‑grade cores.
While no Mineral Resource has yet been declared for Joru, the scale of the system, continuity of mineralisation and geological setting indicate potential for future resource definition, subject to further structural studies and targeted diamond drilling.
