| Reference Type | Journal (article/letter/editorial) |
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| Title | Electron-optical data for crystals of scarbroite |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Brindley, G. W. | Author |
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| Comer, J. J. | Author |
| Year | 1960 (March) | Volume | 32 |
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| Issue | 248 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_32/32-248-363.pdf+ |
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| DOI | doi:10.1180/minmag.1960.032.248.02 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 5548 | Long-form Identifier | mindat:1:5:5548:6 |
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| GUID | 0 |
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| Full Reference | Brindley, G. W., Comer, J. J. (1960) Electron-optical data for crystals of scarbroite. Mineralogical Magazine and Journal of the Mineralogical Society, 32 (248) 363-365 doi:10.1180/minmag.1960.032.248.02 |
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| Plain Text | Brindley, G. W., Comer, J. J. (1960) Electron-optical data for crystals of scarbroite. Mineralogical Magazine and Journal of the Mineralogical Society, 32 (248) 363-365 doi:10.1180/minmag.1960.032.248.02 |
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| In | (1959) Mineralogical Magazine Vol. 32 (248) Mineralogical Society |
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| Abstract/Notes | SummaryElectron micrographs of scarbroite show thin platy crystals of about 1 μ size, having rhombic outlines with angles 66° ± 1° and 113° ± 1°. Single-crystal electron-diffraction patterns show rectangular net patterns, with d100 = 9·90 Å., d010 = 14·67 Å., γ* = 90° ± 0·05°. Strong hk0 reflections show a pseudohexagonal arrangement, but true symmetry is probably orthorhombic or monoclinic. Faces outlining rhombic forms are of type {11l}, . |
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