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


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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.

作者简介

V. Vettegren’

Ioffe Institute

编辑信件的主要联系方式.
Email: Victor.Vettegren@mail.ioffe.ru
俄罗斯联邦, St. Petersburg, 194021

A. Ponomarev

Schmidt Institute of Physics of the Earth

Email: Victor.Vettegren@mail.ioffe.ru
俄罗斯联邦, Moscow, 123242

R. Mamalimov

Ioffe Institute

Email: Victor.Vettegren@mail.ioffe.ru
俄罗斯联邦, St. Petersburg, 194021

I. Shcherbakov

Ioffe Institute

Email: Victor.Vettegren@mail.ioffe.ru
俄罗斯联邦, St. Petersburg, 194021

V. Kulik

Ioffe Institute

Email: Victor.Vettegren@mail.ioffe.ru
俄罗斯联邦, St. Petersburg, 194021

V. Ermakov

Schmidt Institute of Physics of the Earth

Email: Victor.Vettegren@mail.ioffe.ru
俄罗斯联邦, Moscow, 123242

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