Uranium mineralization is hosted, as lenses, in grey sandstones of the "Arenarie della Val Gardena" Fm. of upper Permian age. Associated with U mineralizations are also small quantities of Fe and Cu minerals.
References:
-Campostrini, I., Demartin, F., & Gramaccioli, C. M. (2006). Rio Giulis. Minerali secondari del giacimento uranifero presso Condino, Trento. Rivista Mineralogica Italiana, 30(3), 152-165.
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34 minerals listed.
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