Friction-Induced Changes in the Surface Structure of Basalt and Granite
Friction-induced changes in the structure of the surface layer of basalt and granite samples extracted from a well in the triggered seismicity zone in the Koyna–Warna region, India, have been studied by infrared, Raman, and photoluminescence spectroscopy. It has been found that friction leads to a p...
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Veröffentlicht in: | Physics of the solid state 2018-05, Vol.60 (5), p.975-980 |
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