@article{fdi:010083581,
  title = {{G}ranitic pegmatites as sources of strategic metals},
  author = {{L}innen, {R}. {L}. and {V}an {L}ichtervelde, {M}arieke and {C}erny, {P}.},
  editor = {},
  language = {{ENG}},
  abstract = {{R}are-element granitic pegmatites are well recognized for the diversity and concentrations of metal ores that they host. {T}he supply of some of these elements is of concern, and the {E}uropean {C}ommission recently designated metals such as tantalum and niobium as "critical materials" or "strategic resources." {F}ield relationships, mineral chemistry, and experimental constraints indicate that these elements are concentrated dominantly by magmatic processes. {T}he granitic melts involved in these processes are very unusual because they contain high concentrations of fluxing compounds, which play a key role at both the primary magmatic and metasomatic stages. {I}n particular, the latter may involve highly fluxed melts rather than aqueous fluids.},
  keywords = {strategic ; rare element ; fractionation ; metasomatism ; ore genesis},
  booktitle = {},
  journal = {{E}lements},
  volume = {8},
  numero = {4},
  pages = {275--280},
  ISSN = {1811-5209},
  year = {2012},
  DOI = {10.2113/gselements.8.4.275},
  URL = {https://www.documentation.ird.fr/hor/fdi:010083581},
}