Xenotime in the Lower Buntsandstein of C
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Detlev K. Richter; Holger Krampitz; Peter Görgen; Thomas Götte; Rolf D. Neuser
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Article
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2006
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Elsevier Science
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English
⚖ 572 KB
Xenotime and zircon in heavy mineral separates of siliciclastic sediments can easily be distinguished by means of cathodoluminescence (CL). All shades of bright blue, yellow and grey to white colours have been reported for zircon while only bottle green to greenish yellow colours have been found in