Structural Changes in the Surface of a Heterogeneous Body (Xenolite) under Friction
- 作者: Vettegren’ V.I.1, Ponomarev A.V.2, Mamalimov R.I.1, Shcherbakov I.P.1, Kulik V.B.1, Ermakov V.A.2
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隶属关系:
- Ioffe Institute
- Schmidt Institute of Physics of the Earth
- 期: 卷 60, 编号 10 (2018)
- 页面: 2026-2029
- 栏目: Mechanical Properties, Physics of Strength, and Plasticity
- URL: https://ogarev-online.ru/1063-7834/article/view/204098
- DOI: https://doi.org/10.1134/S1063783418100311
- ID: 204098
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详细
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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