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Friction-Induced Changes in the Surface Structure of Basalt and Granite

  • Mechanical Properties, Physics of Strength, and Plasticity
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Abstract

Friction-induced changes in the structure of the surface layer of basalt and granite samples extracted from a well in the triggered seismicity zone in the Koyna–Warna region, India, have been studied by infrared, Raman, and photoluminescence spectroscopy. It has been found that friction leads to a partial degradation of quartz, albite, and clinopyroxenes crystals. Instead of these crystals, a thin layer of a mineral with a low coefficient of friction—kaolinite—is formed on the surface.

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Authors and Affiliations

  1. Ioffe Institute, St. Petersburg, 194021, Russia

    V. I. Vettegren, R. I. Mamalimov, I. P. Shcherbakov & V. B. Kulik

  2. CSIR National Geophysical Research Institute, Hyderabad, India

    K. Arora

  3. Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, 123242, Russia

    A. V. Ponomarev

Authors
  1. V. I. Vettegren
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  2. K. Arora
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  3. A. V. Ponomarev
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  4. R. I. Mamalimov
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  5. I. P. Shcherbakov
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  6. V. B. Kulik
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Corresponding author

Correspondence to V. I. Vettegren.

Additional information

Original Russian Text © V.I. Vettegren, K. Arora, A.V. Ponomarev, R.I. Mamalimov, I.P. Shcherbakov, V.B. Kulik, 2018, published in Fizika Tverdogo Tela, 2018, Vol. 60, No. 5, pp. 965–969.

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Vettegren, V.I., Arora, K., Ponomarev, A.V. et al. Friction-Induced Changes in the Surface Structure of Basalt and Granite. Phys. Solid State 60, 975–980 (2018). https://doi.org/10.1134/S1063783418050359

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  • DOI: https://doi.org/10.1134/S1063783418050359

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