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Variation in the structure of the surface layer of a heterogeneous solid (gneiss) on a shear

  • Mechanical Properties, Physics of Strength, and Plasticity
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Abstract

The structure of surface layers with a thickness of ~1 μm formed at destruction of gneiss is studied by means of photoluminescent and infrared spectroscopy. It is found that, in this layer, feldspar (plagioclase and microcline) crystals are completely destroyed and replaced by montmorillonite.

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Authors and Affiliations

  1. Ioffe Institute, Russian Academy of Sciences, St. Petersburg, 194021, Russia

    V. I. Vettegren’, R. I. Mamalimov & I. P. Shcherbakov

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

    A. V. Ponomarev

  3. CSIR National Geophysical Research Institute, Hyderabad, Telangana, 500007, India

    K. Arora

  4. Borok Geophysical Observatory, Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Borok, Yaroslavl oblast, 152742, Russia

    A. V. Patonin

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

Correspondence to V. I. Vettegren’.

Additional information

Original Russian Text © V.I. Vettegren’, A.V. Ponomarev, K. Arora, R.I. Mamalimov, I.P. Shcherbakov, A.V. Patonin, 2017, published in Fizika Tverdogo Tela, 2017, Vol. 59, No. 7, pp. 1319–1322.

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Vettegren’, V.I., Ponomarev, A.V., Arora, K. et al. Variation in the structure of the surface layer of a heterogeneous solid (gneiss) on a shear. Phys. Solid State 59, 1345–1348 (2017). https://doi.org/10.1134/S1063783417070319

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  • DOI: https://doi.org/10.1134/S1063783417070319

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