Structural Changes in the Surface of a Heterogeneous Body (Xenolite) under Friction
- Авторлар: Vettegren’ V.I.1, Ponomarev A.V.2, Mamalimov R.I.1, Shcherbakov I.P.1, Kulik V.B.1, Ermakov V.A.2
-
Мекемелер:
- Ioffe Institute
- Schmidt Institute of Physics of the Earth
- Шығарылым: Том 60, № 10 (2018)
- Беттер: 2026-2029
- Бөлім: 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
Дәйексөз келтіру
Аннотация
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.
Авторлар туралы
V. Vettegren’
Ioffe Institute
Хат алмасуға жауапты Автор.
Email: Victor.Vettegren@mail.ioffe.ru
Ресей, St. Petersburg, 194021
A. Ponomarev
Schmidt Institute of Physics of the Earth
Email: Victor.Vettegren@mail.ioffe.ru
Ресей, Moscow, 123242
R. Mamalimov
Ioffe Institute
Email: Victor.Vettegren@mail.ioffe.ru
Ресей, St. Petersburg, 194021
I. Shcherbakov
Ioffe Institute
Email: Victor.Vettegren@mail.ioffe.ru
Ресей, St. Petersburg, 194021
V. Kulik
Ioffe Institute
Email: Victor.Vettegren@mail.ioffe.ru
Ресей, St. Petersburg, 194021
V. Ermakov
Schmidt Institute of Physics of the Earth
Email: Victor.Vettegren@mail.ioffe.ru
Ресей, Moscow, 123242
Қосымша файлдар
