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Liu, Yan, Shigley, James E., Fritsch, Emmanuel, Hemphill, Scott (1995) Relationship between the crystallographic orientation and the ‘alexandrite effect’ in synthetic alexandrite. Mineralogical Magazine, 59 (394) 111-114 doi:10.1180/minmag.1995.59.394.10

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Reference TypeJournal (article/letter/editorial)
TitleRelationship between the crystallographic orientation and the ‘alexandrite effect’ in synthetic alexandrite
JournalMineralogical MagazineISSN0026-461X
AuthorsLiu, YanAuthor
Shigley, James E.Author
Fritsch, EmmanuelAuthor
Hemphill, ScottAuthor
Year1995 (March)Volume59
Issue394
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_59/59-394-111.pdf+
DOIdoi:10.1180/minmag.1995.59.394.10Search in ResearchGate
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Mindat Ref. ID2616Long-form Identifiermindat:1:5:2616:5
GUID0
Full ReferenceLiu, Yan, Shigley, James E., Fritsch, Emmanuel, Hemphill, Scott (1995) Relationship between the crystallographic orientation and the ‘alexandrite effect’ in synthetic alexandrite. Mineralogical Magazine, 59 (394) 111-114 doi:10.1180/minmag.1995.59.394.10
Plain TextLiu, Yan, Shigley, James E., Fritsch, Emmanuel, Hemphill, Scott (1995) Relationship between the crystallographic orientation and the ‘alexandrite effect’ in synthetic alexandrite. Mineralogical Magazine, 59 (394) 111-114 doi:10.1180/minmag.1995.59.394.10
In(1995, March) Mineralogical Magazine Vol. 59 (394) Mineralogical Society
Abstract/NotesAbstractThe transmittance spectra of a synthetic alexandrite recorded along directions parallel to the three crystallographic axes are generally similar, but the observed colour changes along these directions under different light sources are quite different. Calculated hue-angle changes for the colours observed under different pairs of C.I.E. standard illuminants are the largest for light travelling parallel to the a-axis. Therefore, alexandrite should be cut as a gemstone with the top facet oriented parallel to (100) for it to show the most dramatic change in colour.

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