Reference Type | Journal (article/letter/editorial) |
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Title | Geochemistry and EPR of cassiterites from the Iberian Hercynian Massif |
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Journal | Mineralogical Magazine | ISSN | 0026-461X |
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Authors | Murciego, A. | Author |
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Garcla Sanchez, A. | Author |
Dusausoy, Y. | Author |
Martin Pozas, J. M. | Author |
Ruck, R. | Author |
Year | 1997 (June) | Volume | 61 |
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Issue | 406 |
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Publisher | Mineralogical Society |
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Download URL | https://rruff.info/doclib/MinMag/Volume_61/61-406-357.pdf+ |
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DOI | doi:10.1180/minmag.1997.061.406.03Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 176 | Long-form Identifier | mindat:1:5:176:6 |
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GUID | 0 |
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Full Reference | 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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Plain Text | 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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In | (1997, June) Mineralogical Magazine Vol. 61 (406) Mineralogical Society |
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Abstract/Notes | AbstractThis 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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