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

被引：2
|
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 ]
机构：
[1] Russian Acad Sci, Ioffe Inst, St Petersburg 194021, Russia
[2] Russian Acad Sci, Schmidt Inst Phys Earth, Moscow 123242, Russia
来源：
PHYSICS OF THE SOLID STATE | 2018年 / 60卷 / 10期
基金：
俄罗斯基础研究基金会;
关键词：
NANOCRYSTALLINE SOLID SANDSTONE; MG-FE PYROXENES; DYNAMICS; SPECTRA; DESTRUCTION; AMPHIBOLE; MINERALS; DIORITE; LAYER;
D O I：
10.1134/S1063783418100311
中图分类号：
O469 [凝聚态物理学];
学科分类号：
070205 ;
摘要：
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 similar to 60-nm-thick layer of water.
引用
收藏
页码：2026 / 2029
页数：4
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