The uranium mineralization is largely associated with lujavrite, partly altered lavas, hydrothermal analcime veins and pegmatites. Most of the uranium is contained in Steenstrupine and occurs as a disseminated mineral in the lujavrite.
References
- Wyatt J. (2007): The Kvanefjeld Project, El 2005/17, Geological Investigation Pty Ltd. Western Australia 6012
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