Structural changes in a heterogeneous solid (granite) under shock wave action


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Abstract

The structure of two granite types (plagiogranite and alaskite) before and after shock wave action has been studied by infrared, Raman, and photoluminescence spectroscopy methods. It has been found that the shock wave caused transformation of quartz and feldspar crystals composing these granites into diaplectic glasses.

About the authors

V. I. Vettegren

Ioffe Physical-Technical Institute

Author for correspondence.
Email: Victor.Vettegren@mail.ioffe.ru
Russian Federation, ul. Politekhnicheskaya 26, St.Petersburg, 194021

I. P. Shcherbakov

Ioffe Physical-Technical Institute

Email: Victor.Vettegren@mail.ioffe.ru
Russian Federation, ul. Politekhnicheskaya 26, St.Petersburg, 194021

R. I. Mamalimov

Ioffe Physical-Technical Institute

Email: Victor.Vettegren@mail.ioffe.ru
Russian Federation, ul. Politekhnicheskaya 26, St.Petersburg, 194021

V. B. Kulik

Ioffe Physical-Technical Institute

Email: Victor.Vettegren@mail.ioffe.ru
Russian Federation, ul. Politekhnicheskaya 26, St.Petersburg, 194021

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