Friction properties and deformation mechanisms of halite(-mica) gouges from low to high sliding velocities

The evolution of friction as a function of slip rate is important in understanding earthquake nucleation and propagation. Many laboratory experiments investigating friction of fault rocks are either conducted in the low velocity regime (10−8–10−4 ms−1) or in the high velocity regime (0.01–1 m s−1)....

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Veröffentlicht in:	Earth and planetary science letters 2017-01, Vol.458, p.107-119
Hauptverfasser:	Buijze, Loes, Niemeijer, André R., Han, Raehee, Shimamoto, Toshihiko, Spiers, Christopher J.
Format:	Artikel
Sprache:	eng
Schlagworte:	Deformation mechanisms Ductile brittle transition Evolution Friction halite Hardening rate low to high velocity friction Rocks rotary shear apparatus Sliding Slip
Online-Zugang:	Volltext
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