Characterization of natural brannerite: implication for U deposit fingerprints and dating mineralizing events

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00023272%3A_____%2F17%3A10134108" target="_blank" >RIV/00023272:_____/17:10134108 - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Result language
angličtina
Original language name
Characterization of natural brannerite: implication for U deposit fingerprints and dating mineralizing events
Original language description
Uraninite and coffinite are the most frequent U(IV) minerals. Brannerite may be also present, but recovery of uranium is more difficult because brannerite is poorly soluble. These U-Ti oxides are currently found in several deposit types such as intrusive-related, hydrothermal or metamorphic. The combination of textural observations, major and trace elements distribution and U-Pb dating allows to decipher the conditions of their genesis. REE patterns can be used as a specific signature for each deposit type. A better understanding of the formation of natural brannerite could provide precious data for the mining industry (i.e. uranium leaching from brannerite).
Czech name
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Czech description
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Publication year
2017
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Article name in the collection
Mineral resources to discover
ISBN
978-2-9816898-0-1
ISSN
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e-ISSN
neuvedeno
Number of pages
4
Pages from-to
727-730
Publisher name
SOC GEOLOGY APPLIED MINERAL DEPOSITS-SGA, UNIV GENEVA, DEPT EARTH SCI, 11, RUE MARAICHERS, GENEVA 4, CH 1205, SWITZERLAND
Place of publication
Geneva, Švýcarsko
Event location
Quebec, Kanada
Event date
Aug 20, 2017
Type of event by nationality
WRD - Celosvětová akce
UT code for WoS article
000439764100180

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