A microphysical model for strong velocity weakening in phyllosilicate-bearing fault gouges

Previous rotary shear experiments, performed on a halite‐muscovite fault gouge analogue system have shown that the presence of phyllosilicates, under conditions favoring the operation of cataclasis and pressure solution in the matrix phase, can have major effects on the frictional behavior of gouges...

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Veröffentlicht in:	Journal of Geophysical Research: Solid Earth 2007-10, Vol.112 (B10), p.n/a
Hauptverfasser:	Niemeijer, A. R., Spiers, C. J.
Format:	Artikel
Sprache:	eng
Schlagworte:	Earth sciences Earth, ocean, space Exact sciences and technology friction phyllosilicates microphysical model pressure solution
Online-Zugang:	Volltext
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