Abstract
Pyrolytic graphite films prepared by means of microsplitting are studied. In the samples, the alternation of pentagonal and hexagonal symmetry planes is revealed. These graphite crystal states can be classified as mesoscopic fullerene-like structures.
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N. N. Andrianova, V. S. Avilkina, A. M. Borisov, E. S. Mashkova, and E. S. Parilis, Vacuum 86, 1630 (2012).
C. M. Mahoney, Mass Spectrom. Rev. 29, 247 (2010).
J. Han, Y. Son, J.-Y. Lee, H. Kwon, and J.-S. Yeo, Abstracts of Papers, 19th International SIMS Conference (South Korea, 2013).
A. K. Geim, Usp. Fiz. Nauk 181 (12), 1284 (2011)
K. S. Novoselov, Usp. Fiz. Nauk 181, 1299 (2011).
P. B. Sorokin and L. A. Chernozatonskii, Phys.—Usp. 56, 105 (2011).
P. M. Coelho, A. Malachias, L. Malard, and R. Magalhães-Paniago, Abstracts of Papers, 11th International SBPMat Conference (Brazil, 2012).
V. V. Korablev, Auger Electron Spectroscopy (Politekhn. Inst., Leningrad, 1973) [in Russian].
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Borisowskiy, P.A., Moos, E.N. & Rudenko, A.I. Features of the crystalline state of graphite layers. J. Surf. Investig. 11, 135–137 (2017). https://doi.org/10.1134/S1027451017010062
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DOI: https://doi.org/10.1134/S1027451017010062