The structural aspects of the Mada Younger Granite complex differ from those described from other ring complexes in the province. Ring-dykes and cauldron subsidence structures are not observed and the extrusive rhyolites do not appear to be related to a volcanic cauldron. The minor remnants of the extrusive rocks were domes over small vents since there are no clear indications of any unified volcanic structure. Volcanic eruptions may have taken place from dispersed vents probably including pipes and fissures. Linear intrusive structures have been observed and there is no concentric arrangement of rock units. The biotite granites appear more as sheet structures dipping gently to the south. Petrographically, the extrusive rocks are rhyolites, the comenditic ignimbrite being distinctly peralkaline with aegirine and arfvedsonite. The granite cupolas may be classified as ‘A’-type and have been affected by pervasive potash metasomatism which caused recrystallization with microline and finely twinned clear euhedral albite, together with mica compositions between annite towards lithian siderophyllite. This process also introduced minerals like fluorite, cassiterite, columbite and thorite which make the Mada complex a possible source for economic minerals.