| Reference Type | Journal (article/letter/editorial) |
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| Title | New determinations of tin and tungsten in granites from south-west England |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Alderton, D. H. M. | Author |
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| Moore, F. | Author |
| Year | 1981 (September) | Volume | 44 |
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| Issue | 335 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_44/44-335-354.pdf+ |
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| DOI | doi:10.1180/minmag.1981.044.335.18Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 3283 | Long-form Identifier | mindat:1:5:3283:8 |
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| GUID | 0 |
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| Full Reference | Alderton, D. H. M., Moore, F. (1981) New determinations of tin and tungsten in granites from south-west England. Mineralogical Magazine, 44 (335) 354-356 doi:10.1180/minmag.1981.044.335.18 |
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| Plain Text | Alderton, D. H. M., Moore, F. (1981) New determinations of tin and tungsten in granites from south-west England. Mineralogical Magazine, 44 (335) 354-356 doi:10.1180/minmag.1981.044.335.18 |
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| In | (1981, September) Mineralogical Magazine Vol. 44 (335) Mineralogical Society |
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| Abstract/Notes | Recent studies on the development of Sn-W mineralization in south-west England (Sheppard, 1977; Simpson et al., 1979; Jackson et al., 1979) indicate that the hydrothermal fluids dominantly consisted of local meteoric waters. These waters were heated up and drawn into the granite in a convective hydrothermal system. It is proposed that the fluids leached Sn and W from minerals such as the dark micas, during their passage through the granite. These metals were then deposited in veins at higher levels in the system. |
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