Metamict zircon from Mozambique
Metamict zircon from granite pegmatites of Zambézia, Mozambique has been studied by annealing, microprobe, X-ray diffraction, DT and TG analysis, and IR spectroscopy. The specimens are contaminated by epitaxially intergrown xenotime. It is presumed that the lanthanoides, occur in the xenotime phase...
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Format: | Article |
Language: | English |
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Geological Society of Finland
1985-12-01
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Series: | Bulletin of the Geological Society of Finland |
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Online Access: | http://www.geologinenseura.fi/bulletin/Volume57/sgs_bt_057_pages_181_195.pdf |