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• W1934524791 abstract "Uranium-rich zircons from a Paleoproterozoic, high-grade deformation zone in the Fennoscandian Shield, central Sweden, show an almost complete resetting of the U-Pb system in early Phanerozoic time. A mylonitic gneiss in the deformation zone contains two types of highly discordant (>70%), U-rich zircons: large, brown, cloudy prisms, and small milky-white irregularly shaped grains. The gneiss also contains mostly clear prismatic zircon of lower U content with mildly discordant to concordant U-Pb ages. Laser Raman spectroscopy reveals that the dark cathodoluminescent areas in brown zircons have a highly metamict crystal structure, whereas the structures of both the dark cathodoluminescent milky-white grains and the bright cathodoluminescent clear prisms have higher degrees of crystallinity." @default.
• W1934524791 created "2016-06-24" @default.
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• W1934524791 date "2001-04-01" @default.
• W1934524791 modified "2023-10-18" @default.
• W1934524791 title "Low<i>P</i>-<i>T</i>Caledonian resetting of U-rich Paleoproterozoic zircons, central Sweden" @default.
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• W1934524791 doi "https://doi.org/10.2138/am-2001-0416" @default.
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