Abstract
The structure of marble fracture fragments formed after the destruction under the action of a shock wave have been analyzed by Raman, infrared, and luminescence spectroscopic techniques. It has been found that calcite I in the surface layer of fragments with thicknesses of about 2 μm is transformed into high-pressure phase calcite III. At the same time, concentrations of Mn2+, Eu3+, and other ions decrease to about onefourth of their initial values.
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Original Russian Text © I.P. Shcherbakov, V.I. Vettegren, A.Ya. Bashkarev, R.I. Mamalimov, 2018, published in Zhurnal Tekhnicheskoi Fiziki, 2018, Vol. 88, No. 1, pp. 80–84.
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Shcherbakov, I.P., Vettegren, V.I., Bashkarev, A.Y. et al. Transformation of the Surface Structure of Marble under the Action of a Shock Wave. Tech. Phys. 63, 78–82 (2018). https://doi.org/10.1134/S106378421801022X
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DOI: https://doi.org/10.1134/S106378421801022X