Other
Scientific paper
Mar 1969
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1969gecoa..33..417g&link_type=abstract
Geochimica et Cosmochimica Acta, vol. 33, Issue 3, pp.417-420
Other
Scientific paper
Bi has been estimated spectrochemically in 29 specimens of gadolinite; it varies from 12 to 262 ppm and averages at 63 ppm. The presence of distinct traces of Bi in gadolinite is evidently due to the ability of Bi 3+ to replace rare earth cations in the gadolinite structure. Some approximate observations have also been made on the Bi concentration in other rare earth minerals and in apatite.
Ahrens L. H.
Gurney John J.
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