Find of anisotropic carbonic matter on a curve-faced diamond crystal


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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.

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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