Abstract
Results of the study of carbon material (CM) discovered in kimberlite-like rocks of the Charteskii Complex (Subpolar Urals) are considered. It is shown that CM is represented by partially oxidized graphite and optically transparent amorphous CM (presumably diamond-like carbon). The data obtained are important for estimation of the diamond potential of this object, as well as for understanding of the new mechanism of the formation of diamond-like carbon and diamond.
Similar content being viewed by others
References
L. I. Luk’yanova and A. V. Bel’skii, Sov. Geol., No. 1, 93 (1987).
Tectonic Zoning and Minerageny of the Urals (Analytical Review) (Geokart. GEOS, Moscow, 2006), p. 180 [in Russian].
I. I. Golubeva and T. G. Shumilova, Vestnik Instituta Geologii Komi Nauchnogo Tsentra UrO RAN, No. 11, 27 (2013).
P. H. Tan, S. Dimovski, and Yu. Gogotsi, Phil. Trans. R. Soc. Lond. A 362, 2289 (2004).
J. Campos-Delgado, J. M. Romo-Herrera, X. Jia, et al., Nano Lett. 8 (9), 2773 (2008).
W. Ren, R. Saito, L. Gao, et al., Phys. Rev. B, No. 81, 035412 (2010).
R. Saito, M. Furukawa, G. Dresselhaus, et al., J. Phys.: Condens. Matter, No. 22, 334203 (6) (2010).
A. M. Zaitsev, Optical properties of diamond: A data handbook (Springer, Berlin, 2001).
A. C. Ferrari and J. Robertson, Phil. Trans. R. Soc. Lond. A 362, 2477 (2004).
J. Schwan, S. Ulrich, V. Batori, et al., J. Appl. Phys. 80 (1), 440 (1996).
K. A. Mkhoyan, A. W. Contryman, J. Silcox, et al., Nano Lett. 9 (3), 1058 (2009).
D. R. McKenzie, Rep. Prog. Phys., No. 59, 1611 (1996).
Author information
Authors and Affiliations
Corresponding author
Additional information
Original Russian Text © S.I. Isaenko, T.G. Shumilova, S.S. Shevchuk, 2015, published in Doklady Akademii Nauk, 2015, Vol. 464, No. 5, pp. 603–607.
Rights and permissions
About this article
Cite this article
Isaenko, S.I., Shumilova, T.G. & Shevchuk, S.S. Carbon matter in kimberlite-like rocks of the Charteskii Complex (Subpolar Urals). Dokl. Earth Sc. 464, 1062–1065 (2015). https://doi.org/10.1134/S1028334X1510013X
Received:
Published:
Issue Date:
DOI: https://doi.org/10.1134/S1028334X1510013X