| Reference Type | Journal (article/letter/editorial) |
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| Title | An occurrence of phlogopite and its transformation to vermiculite by weathering |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Smith Aitken, W. W. | Author |
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| Year | 1965 (March) | Volume | 35 |
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| Issue | 269 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_35/35-269-151.pdf+ |
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| DOI | doi:10.1180/minmag.1965.035.269.18Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 5854 | Long-form Identifier | mindat:1:5:5854:8 |
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| GUID | 0 |
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| Full Reference | Smith Aitken, W. W. (1965) An occurrence of phlogopite and its transformation to vermiculite by weathering. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (269) 151-164 doi:10.1180/minmag.1965.035.269.18 |
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| Plain Text | Smith Aitken, W. W. (1965) An occurrence of phlogopite and its transformation to vermiculite by weathering. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (269) 151-164 doi:10.1180/minmag.1965.035.269.18 |
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| In | (1965) Mineralogical Magazine Vol. 35 (269) Mineralogical Society |
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| Abstract/Notes | SummaryThe characteristics of a phlogopite and its weathering product, vermiculite, have been studied by X-ray, infra-red, electron-microscope, and chemical methods. Inclusions within these minerals have been identified as thin films rich in iron oxide (which impart a schiller effect), spinel (which may exist in a preferred orientation), and serpentine. The orientation relationship between the fresh mica and its weathering product has been established by single-crystal methods. The mechanism of transformation from a 1-layer to a 2-layer polytype is discussed. |
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