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SEM EDS at the National Museum of Wales.
a rare member of the xenotime group of minerals known from just a few localities worldwide. Typically chernovite-(Y) occurs in altered rhyolites, in pegmatite, or within "Alpine-type" veins.
Kerbey (2013) described minute spots of chernovite-(Y) with dravite in green reduction spots in lower Cambrian slates from Alexandra Quarry, Gwynedd.
Journal of the Russell Society, 16, 60-63.