Structural Changes in the Surface of a Heterogeneous Body (Xenolite) under Friction


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Resumo

The structure of the surface layer of a heterogeneous solid body (xenolite) before and after friction is studied by infrared and Raman spectroscopy. Before friction, the layer contained hornblende and pyroxene crystals. The friction resulted in partial transformation of pyroxenes into hornblende and the latter was transformed into montmorillonite clay. The xenolite surface is covered with a ~60-nm-thick layer of water.

Sobre autores

V. Vettegren’

Ioffe Institute

Autor responsável pela correspondência
Email: Victor.Vettegren@mail.ioffe.ru
Rússia, St. Petersburg, 194021

A. Ponomarev

Schmidt Institute of Physics of the Earth

Email: Victor.Vettegren@mail.ioffe.ru
Rússia, Moscow, 123242

R. Mamalimov

Ioffe Institute

Email: Victor.Vettegren@mail.ioffe.ru
Rússia, St. Petersburg, 194021

I. Shcherbakov

Ioffe Institute

Email: Victor.Vettegren@mail.ioffe.ru
Rússia, St. Petersburg, 194021

V. Kulik

Ioffe Institute

Email: Victor.Vettegren@mail.ioffe.ru
Rússia, St. Petersburg, 194021

V. Ermakov

Schmidt Institute of Physics of the Earth

Email: Victor.Vettegren@mail.ioffe.ru
Rússia, Moscow, 123242

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