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Combined in-situ U–Pb, Lu–Hf and trace element LA–ICP–MS analyses were performed on zircons from the W-mineralized K1–K3 orthogneiss and associated aplite gneiss from the Felbertal scheelite deposit. The textural and trace element characteristics suggest the presence of magmatic and hydrothermal zircon. Magmatic zircons have low concentrations of W (0.108–3.77ppm), Nb (5.04–48ppm), U (691–3079ppm),...
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