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Deposits of this type consist of disseminations and veins of uraninite/pitchblendc in volcanic rocks that are commonly felsic and subalkaline to peralkaline felsic in composition, but some potassic alkaline mafic to intermediate rocks also host uranium occurrences. The volcanic rocks are formed mainly in late- or postorogenic settings and continental extensional tectonic environments . They occur in all volcanic lithofacies, from proximal to distal in setting, including volcaniclastic sediments. Molybdenum, flourine, thorium, rare-earth elements , and lead-zinc, are commonly enriched in the deposits and may be of economic importance.

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