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Whittaker, E. J. W., Cressey, B. A., Hutchison, J. L. (1981) Edge dislocations in fibrous grunerite. Mineralogical Magazine, 44 (335) 287-291 doi:10.1180/minmag.1981.044.335.08

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Reference TypeJournal (article/letter/editorial)
TitleEdge dislocations in fibrous grunerite
JournalMineralogical MagazineISSN0026-461X
AuthorsWhittaker, E. J. W.Author
Cressey, B. A.Author
Hutchison, J. L.Author
Year1981 (September)Volume44
Issue335
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_44/44-335-287.pdf+
DOIdoi:10.1180/minmag.1981.044.335.08Search in ResearchGate
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Mindat Ref. ID3273Long-form Identifiermindat:1:5:3273:9
GUID0
Full ReferenceWhittaker, E. J. W., Cressey, B. A., Hutchison, J. L. (1981) Edge dislocations in fibrous grunerite. Mineralogical Magazine, 44 (335) 287-291 doi:10.1180/minmag.1981.044.335.08
Plain TextWhittaker, E. J. W., Cressey, B. A., Hutchison, J. L. (1981) Edge dislocations in fibrous grunerite. Mineralogical Magazine, 44 (335) 287-291 doi:10.1180/minmag.1981.044.335.08
In(1981, September) Mineralogical Magazine Vol. 44 (335) Mineralogical Society
Abstract/NotesAbstractSections perpendicular to [001] of ion-thinned specimens of fibrous grunerite (amosite) have been examined by high-resolution transmission electron microscopy. In this orientation, two kinds of dislocation have been observed with about equal frequency. One lies on [001] and has a Burgers vector a. The other is on [001] and has a Burgers vector ½a+½b Interpretation of features associated with these dislocations has been assisted by the use of two-dimensional models of I-beam cross-sections which can be interlocked to simulate the possible modes of stacking.


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