SYNTHESIS OF FELDSPAR BICRYSTALS BY DIRECT BONDING

dc.contributor.authorHeinemann S.
dc.contributor.authorWirth R.
dc.contributor.authorDresen G.
dc.date.accessioned2021-03-15T07:09:53Z
dc.date.available2021-03-15T07:09:53Z
dc.date.issued2001
dc.description.abstractWe have produced synthetic feldspar bicrystals using a direct bonding technique. A gem-quality orthoclase crystal from Itrongay, Madagascar, was used for the bonding experiments. Microprobe analysis shows only minor concentrations of iron and sodium. Orthoclase single crystal plates oriented parallel (0 0 1) were cut and chemomechanically polished with silica slurry. From interferometry, final roughness of the square crystal plates was about 0.34 nm. Specimens were wet-chemically cleaned using deionised water. The bonding procedure produced an orthoclase bicrystal with an optically straight grain boundary-oriented parallel (0 0 1), which was investigated by HREM. Along the interface no amorphous layer was observed between lattice fringes of both crystals. We suggest that the bicrystals formed by initial hydrogen bonding and subsequent water loss and polymerisation of silanol and aluminol groups at elevated temperatures.
dc.identifierhttps://www.elibrary.ru/item.asp?id=816723
dc.identifier.citationPhysics and Chemistry of Minerals, 2001, 28, 10, 685-692
dc.identifier.issn0342-1791
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/26718
dc.subjectBICRYSTAL SYNTHESIS
dc.subjectFELDSPAR
dc.subjectDIRECT BONDING
dc.subjectGRAIN BOUNDARY
dc.titleSYNTHESIS OF FELDSPAR BICRYSTALS BY DIRECT BONDING
dc.typeСтатья

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