Physics
Scientific paper
Jun 1988
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1988gecoa..52.1497m&link_type=abstract
Geochimica et Cosmochimica Acta, vol. 52, Issue 6, pp.1497-1503
Physics
4
Scientific paper
The interpretation of (i) the interelement relationships of (Ta + Nb) and W or (Fe + Mn), (ii) Mössbauer spectrometric results on the oxidation state of Fe, and (iii) electron probe microanalysis of cassiterites reveal that coupled substitutions of the type 2 ( Ta , Nb ) 5+ + ( Fe , Mn ) 2+ = 3 Sn 4+ W 6+ + 2 Fe 3+ = 3 Sn 4+ Fe 3+ + OH - = Sn 4+ + O 2- are dominant at least at the temperatures of formation of cassiterite. Additional replacements such as ( Ta , Nb ) 4+ = Sn 4+ cannot be ruled out. Aspects of the structural control on trace element distribution, and maintenance of electroneutrality of the crystal lattice are discussed.
Dulski Peter
Malow G.
Moller Palle
Riedel Eberhard
Szacki W.
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