| Reference Type | Journal (article/letter/editorial) |
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| Title | A transmission electron microscope and X-ray diffraction study of muscovite and chlorite |
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| Journal | Mineralogical Magazine |
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| Authors | Oertel, G. | Author |
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| Curtis, C. D. | Author |
| Phakey, P. P. | Author |
| Year | 1973 (June) | Volume | 39 |
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| Issue | 302 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_39/39-302-176.pdf+ |
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| DOI | doi:10.1180/minmag.1973.039.302.05Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 6665 | Long-form Identifier | mindat:1:5:6665:9 |
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| GUID | 0 |
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| Full Reference | Oertel, G., Curtis, C. D., Phakey, P. P. (1973) A transmission electron microscope and X-ray diffraction study of muscovite and chlorite. Mineralogical Magazine, 39 (302) 176-188 doi:10.1180/minmag.1973.039.302.05 |
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| Plain Text | Oertel, G., Curtis, C. D., Phakey, P. P. (1973) A transmission electron microscope and X-ray diffraction study of muscovite and chlorite. Mineralogical Magazine, 39 (302) 176-188 doi:10.1180/minmag.1973.039.302.05 |
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| In | (1973, June) Mineralogical Magazine Vol. 39 (302) Mineralogical Society |
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| Abstract/Notes | SummarySingle-crystal diffraction patterns produced by transmitted radiation, both X-rays and electrons, reveal varying degrees of disorder and long-range order in common phyllosilicates from several different rock types. The transmission electron micrographs and their selected-area diffraction patterns demonstrate the presence of numerous stacking faults parallel to (001) of muscovite and chlorite. Individual stacking faults can be recognized by the diffraction-contrast fringe patterns they cause, and partial dislocations can be seen where such faults terminate inside a crystal. Long-range order of muscovite explains what seemed to be spurious, high ‘background’ levels that are sometimes encountered in the analysis of rock fabrics by transmitted X-rays. |
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