A specimen of foam graphite foil is shown to have an anisotropic structure and consist of layers (stacks) of crystallite sheets weakly bound to one another.
S. I. Kudryashov, S. V. Sokolov, N. B. Zorov, A. A. Karabutov and Y. Y. Kuzyakov, Mendeleev Commun., 1997, 7, 25 DOI: 10.1070/MC1997v007n01ABEH000658
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