Abstract
The composition, structure, and morphology of iron-containing diamond–kimberlite contact sites were studied by means of scanning electron microscopy and Raman spectroscopy. The data obtained confirm the hypothesis of the similarity of mechanisms of diamond formation in nature and in experiments.
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Original Russian Text © V.L. Skvortsova, M.I. Samoylovich, A.F. Belyanin, 2015, published in Doklady Akademii Nauk, 2015, Vol. 465, No. 3, pp. 343–346.
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Skvortsova, V.L., Samoylovich, M.I. & Belyanin, A.F. Studies of phase composition of contact sites of diamond crystals and the surrounding rocks. Dokl. Earth Sc. 465, 1187–1190 (2015). https://doi.org/10.1134/S1028334X15110215
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DOI: https://doi.org/10.1134/S1028334X15110215