| Locality type: | Massif |
| Classification |
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| Species: | Fergusonite-(Ce) |
| Formula: | CeNbO4 · 0.3H2O |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Fergusonite-(Ce) data |
| Locality Data: | Click here to view Khaldzan Buragtag massif, Myangad District, Khovd Province, Mongolia |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 1571860 |
| Long-form Identifier: | 1:3:1571860:8 |
| GUID (UUID V4): | 97b3c28c-fb21-411d-b6eb-c0b5510e809d |
| Localities for Fergusonite-(Ce) in this Region |
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| Tsakhirin Khuduk Y-Zr-Nb deposit, Khaldzan Buragtag massif, Myangad District, Khovd Province, Mongolia |
| Nearest other occurrences of Fergusonite-(Ce) |
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| 14.2km (8.8 miles) | ⓘTsakhirin Khuduk Y-Zr-Nb deposit, Khaldzan Buragtag massif, Myangad District, Khovd Province, Mongolia |
| References |
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Bagiński, B., Jokubauskas, P., Domańska-Siuda, J., Kartashov, P., & Macdonald, R. (2016). Hydrothermal metasomatism of a peralkaline granite pegmatite, Khaldzan Buragtag massif, Mongolian Altai |
| Reference Search (possible matching items) |
|---|
 | | Journal (article/letter/editorial) | | with chevkinite-(Ce) in a quartz-epidote metasomatite; (2) during alteration of monazite(Ce) in a quartzolite;...of fergusonite-(Y) in a quartz-epidote metasomatite; (4) following exsolution from chevkinite-(Ce); and...and (5) associated with cerite-(Ce) and with ilmenite and bastnäsite-(Ce) in late-stage veinlets in a syenitic...(the Keivy massif, Kola Peninsula and the Vishnevye Mountains, southern Urals) and Mongolia (the Khaldzan-Buragtag...composition and hydrothermal alteration of chevkinite-(Ce), references also being given in Table 1. Numerous |  | | Journal (article/letter/editorial) | | fractionation during crystallization and alteration of fergusonite-(Y) from Zr-REE-Nb–rich late- to post-magmatic...fractionation during crystallization and alteration of fergusonite-(Y) from Zr-REE-Nb–rich late- to post-magmatic...fractionation during crystallization and alteration of fergusonite-(Y) from Zr-REE-Nb–rich late- to post-magmatic...have abundant fergusonite-(Y) mineralization. More than 90 EPMA analyses of fergusonite-(Y) from different...Variations in Y/HREE ratio during growth of fergusonite-(Y) in a pegmatite are explained by a change |
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