Find of anisotropic carbonic matter on a curve-faced diamond crystal
- Authors: Brodskaya R.L.1, Golubev E.A.2, Isaenko S.I.2
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Affiliations:
- Karpinsky Russian Geological Research Institute
- Institute of Geology, Komi Science Center, Ural Branch
- Issue: Vol 58, No 8 (2016)
- Pages: 623-627
- Section: Article
- URL: https://ogarev-online.ru/1075-7015/article/view/215116
- DOI: https://doi.org/10.1134/S1075701516080043
- ID: 215116
Cite item
Abstract
The study focuses on the identification and investigation of crystal-optical anisotropy phenomena observed on surfaces of a curve-faced diamond crystal found in alluvial sediments of the Lower Us’va River in Perm territory. Raman spectroscopy and atomic force microscopy show that interference of polarized light reflected from the tetrahexahedral faces of the diamond crystal is inspired by anisotropic carbonic matter, which appears as a film with graphene or nanographite structure and about 4 nm in thickness. The data allow us to suggest the formation conditions of curve-faced diamond crystals and origin of nanocrystalline carbonic matter on their faces.
Keywords
About the authors
R. L. Brodskaya
Karpinsky Russian Geological Research Institute
Author for correspondence.
Email: rimma_brodskaya@vsegei.ru
Russian Federation, Srednii pr. 74, St. Petersburg, 199106
E. A. Golubev
Institute of Geology, Komi Science Center, Ural Branch
Email: rimma_brodskaya@vsegei.ru
Russian Federation, Pervomaiskaya ul. 54, Syktyvkar, Komi Republic, 167982
S. I. Isaenko
Institute of Geology, Komi Science Center, Ural Branch
Email: rimma_brodskaya@vsegei.ru
Russian Federation, Pervomaiskaya ul. 54, Syktyvkar, Komi Republic, 167982
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