Single microcrystals of Li2CO3 (zabuyelite) were observed on {0001} calcite surfaces, epitaxially grown and oriented along the <210> directions of calcite, the {001} form of zabuyelite being by far the best candidate to form the epitaxial interface. In addition, 3-fold pseudotwins of zabuyelite were observed in epitaxy on the cleavage {101j4} rhombohedron surface of calcite. The new twinning law is described along with the most probable zabuyelite/calcite interface. Further, a general rule is proposed, concerning the conservation of the orientation of the carbonate groups across the epitaxial interfaces and twin boundaries in carbonates.

Single and Twinned Li2CO3 Crystals (Zabuyelite) Epitaxially Grown on {0001} and {10-14} Forms of CaCO3 (Calcite) Crystals

MASSARO, Francesco Roberto;PASTERO, Linda;COSTA, Emanuele;AQUILANO, Dino
2008-01-01

Abstract

Single microcrystals of Li2CO3 (zabuyelite) were observed on {0001} calcite surfaces, epitaxially grown and oriented along the <210> directions of calcite, the {001} form of zabuyelite being by far the best candidate to form the epitaxial interface. In addition, 3-fold pseudotwins of zabuyelite were observed in epitaxy on the cleavage {101j4} rhombohedron surface of calcite. The new twinning law is described along with the most probable zabuyelite/calcite interface. Further, a general rule is proposed, concerning the conservation of the orientation of the carbonate groups across the epitaxial interfaces and twin boundaries in carbonates.
2008
8 (6)
2041
2046
F.R. Massaro; L. Pastero; E. Costa;† G. Sgualdino; D. Aquilano
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2318/101093
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