Abstract
"The davidites, which occur disseminated in Archaean schists and granulites, exhibit a number of interesting microtextures and show a wide variation in U 3 O 8 content. In one instance the uranium content appears to be shared between davidite and ilmenite with which the former is intergrown. Field evidence together with an unusually diverse variety of trace elements indicate a geosynclinal origin for the davidite and associated minerals."
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