L.K. Wang, A. Acovic, et al.
MRS Spring Meeting 1993
Chemical analysis of ‘voidites’ in diamond reveals only nitrogen, whereas similar analysis of ‘platelets’ shows no detectable nitrogen. The method of analysis is electron energy-loss spectroscopy in a dedicated scanning transmission electron microscope. The voidite size ranges from 2 to 5 nm. The results suggest that the voidites arise from discontinuous precipitation of nitrogen on dislocations including dislocations bounding the platelets. The nitrogen in the voidites is very dense (one-half the atomic density of the diamond) and it seems probable that the diamonds are formed somewhat deeper in the Earth's mantle than previously estimated. © 1989 Taylor & Francis Group, LLC.
L.K. Wang, A. Acovic, et al.
MRS Spring Meeting 1993
R.W. Gammon, E. Courtens, et al.
Physical Review B
R.J. Gambino, N.R. Stemple, et al.
Journal of Physics and Chemistry of Solids
P. Alnot, D.J. Auerbach, et al.
Surface Science