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Murciego, A., Garcla Sanchez, A., Dusausoy, Y., Martin Pozas, J. M., Ruck, R. (1997) Geochemistry and EPR of cassiterites from the Iberian Hercynian Massif. Mineralogical Magazine, 61 (406) 357-365 doi:10.1180/minmag.1997.061.406.03

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Reference TypeJournal (article/letter/editorial)
TitleGeochemistry and EPR of cassiterites from the Iberian Hercynian Massif
JournalMineralogical MagazineISSN0026-461X
AuthorsMurciego, A.Author
Garcla Sanchez, A.Author
Dusausoy, Y.Author
Martin Pozas, J. M.Author
Ruck, R.Author
Year1997 (June)Volume61
Issue406
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_61/61-406-357.pdf+
DOIdoi:10.1180/minmag.1997.061.406.03Search in ResearchGate
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Mindat Ref. ID176Long-form Identifiermindat:1:5:176:6
GUID0
Full ReferenceMurciego, A., Garcla Sanchez, A., Dusausoy, Y., Martin Pozas, J. M., Ruck, R. (1997) Geochemistry and EPR of cassiterites from the Iberian Hercynian Massif. Mineralogical Magazine, 61 (406) 357-365 doi:10.1180/minmag.1997.061.406.03
Plain TextMurciego, A., Garcla Sanchez, A., Dusausoy, Y., Martin Pozas, J. M., Ruck, R. (1997) Geochemistry and EPR of cassiterites from the Iberian Hercynian Massif. Mineralogical Magazine, 61 (406) 357-365 doi:10.1180/minmag.1997.061.406.03
In(1997, June) Mineralogical Magazine Vol. 61 (406) Mineralogical Society
Abstract/NotesAbstractThis paper is based on microprobe analysis (Ta, Nb, Fe, Mn, Ti, W, Sn) and Fe3+ EPR spectra of cassiterite samples from 14 tin deposits from the Iberian Hercynian Massif. The interpretation of microprobe data, atomic ratios (Fe+Mn)/(Nb+Ta), and Fe3+ EPR spectra reveal that the coupled substitution: 3Sn4+ = (Fe,Mn)2+ + 2(Nb,Ta)5+ is dominant in cassiterites from pegmatites, and high-temperature quartz veins and in the dark zones of cassiterites.The mechanisms:2Sn4+ = Fe3+ + (Nb,Ta)5+ andSn4+ + O2− = Fe3+ + OH−are dominant in those from medium-low temperature quartz veins and in the light zones of cassiterites.


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