Reference Type | Journal (article/letter/editorial) |
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Title | Orientation of the boundaries of out-of-step domains in anorthite |
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Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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Authors | Ribbe, Paul H. | Author |
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Colville, Alan A. | Author |
Year | 1968 (June) | Volume | 36 |
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Issue | 282 |
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Publisher | Mineralogical Society |
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Download URL | https://rruff.info/doclib/MinMag/Volume_36/36-282-814.pdf+ |
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DOI | doi:10.1180/minmag.1968.036.282.08Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 6160 | Long-form Identifier | mindat:1:5:6160:9 |
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GUID | 0 |
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Full Reference | Ribbe, Paul H., Colville, Alan A. (1968) Orientation of the boundaries of out-of-step domains in anorthite. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (282) 814-819 doi:10.1180/minmag.1968.036.282.08 |
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Plain Text | Ribbe, Paul H., Colville, Alan A. (1968) Orientation of the boundaries of out-of-step domains in anorthite. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (282) 814-819 doi:10.1180/minmag.1968.036.282.08 |
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In | (1966) Mineralogical Magazine Vol. 36 (282) Mineralogical Society |
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Abstract/Notes | SummaryThe orientation of the boundaries of out-of-step domains in ‘transitional’ anorthite has been deduced from the direction of elongation of the diffuse X-ray reflections h + h + l = 2n + 1 in selected precession photographs. The reflections are elongated normal to which is in the zone and contains the body-centring vector (a+b−c)/2. The structure is presumed to be perfect parallel to . Atoms in essentially identical, primitive anorthite-like domains are related across the out-of-step domain boundaries by body-centring vectors. Increasing diffuseness of the h + k + l = 2n + 1 reflections indicates progressively smaller domains (more frequent domain boundaries), and when thesereflections disappear, the structure has become body-centred on the average. |
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